Major geological features of Yinshan mountains: from craton to composite orogenic regions
-
摘要:
阴山山脉位于东亚大陆腹地，该区地壳以大面积出露前寒武纪早期的变质杂岩和晚古生代及中生代的岩浆岩，发育上盘向南和向北的多期逆掩推覆构造为主要地质特征。在早期的文献中，该山脉被作为中朝准地台（华北克拉通的同义词）的组成部分，意在其与典型的地台不同。在20世纪后期，该区中生代的岩浆活动和构造变形被归因于板内或陆内造山作用，晚古生代的岩浆活动被归因于与古亚洲洋演化有关的陆缘增生和陆间碰撞造山作用。但是几乎所有文献都认为该区是华北克拉通的组成部分。该区究竟是克拉通还是造山带，如果是造山带，是如何从克拉通转变为造山带的？这不仅是个区域地质构造问题，更重要的是，还与古老大陆地壳保存和再造这一大陆动力学问题密切相关，而且还涉及能否正确认识该区的资源潜力。本文基于已有的岩浆活动和构造变形资料，将该山脉自北向南划分为3个构造单元，北部单元为古华北克拉通北缘的早古生代陆缘增生造山带，中部单元为泥盆纪—三叠纪陆缘活化造山带，南部单元为侏罗纪—白垩纪陆内活化造山带。中部单元经过泥盆纪—三叠纪岩浆活动和二叠纪—三叠纪构造变形，由克拉通转变为造山带；南部单元在侏罗纪—白垩纪历经2个伸展-收缩构造变形旋回，由克拉通转变为造山带。据此得出，该山脉地壳主体从早白垩世晚期开始转变为由北亚造山区南部和东亚造山区西缘构成的复合造山区，不再具有克拉通的构造属性。同时，首次发表了北部单元构造变形和中部单元白云鄂博群构造变形的新资料，提出了现今阴山山脉地貌特征形成于新生代晚期，在早古生代晚期、古生代末期、侏罗纪晚期和早白垩世晚期该区发生了多次大规模地壳缩短，中部单元可以划分为4个亚带，白云鄂博群遭受了早期紧闭褶皱、中期左行走滑和晚期上盘向北逆冲3个阶段的构造变形；南部单元强烈逆掩推覆主要发生在早白垩世晚期等新认识。最后，对该区需要进一步研究的主要地质构造问题提出了初步认识。
Abstract:The Yinshan mountains is located in the interior of the eastern Asian continent and is mainly characterized by the exposure of a large area of the Early Precambrian, including the Neo−Archean and Paleo−Proterozoic metamorphosed complexes and late Paleozoic and Triassic plutons, and by multi−age thrusting tectonics with south− and north−verging movement. In the early publications, the mountains was considered as part of so−called Sino−Korean paraplatform, which is considered as same−meaning term with North China craton, implying its difference from the typical platform on the Earth. Since 1990’s, Mesozoic magmatism and structural deformation has been related to within−plate or intracontinental orogeny, and late Paleozoic magmatic rocks to the Andes−type of orogeny in the southern continental margin of the Paleo−Asian ocean between the North China in the south and Siberian platform in the north. However, the mountains have been still considered as part of North China Craton almost in all of publications, implying no change of its tectonic affinity. Whether the mountain is part of the craton or not, how it was changed from the Craton into the orogenic belt if it is not, is not only a regional or local tectonic issue, but also ones relating closely to the evolution of the continental dynamics, and deals with the scientific access of resource potentials. In this paper, the mountains is divided into three tectonic units based on available data both of magmatic rocks and structural deformation. The north unit is part of the island–arc type of an accreted orogenic belt adjacent to the northern margin of the ancient North China craton during the Early Paleozoic, the central one is an activated orogenic belt on the basis of and by the activation of the northern marginal part of the Craton from the Devonian to Triassic, and the south is part of an intracontinental activated orogenic one in the interior of the Craton in the period from the Jurassic to Early Cretaceous. It is further clearly stated that the central unit was changed from the craton into the orogenic belt by Devonian to Triassic magmatism and Permian to Triassic structural deformation, and that the south by two extension−compression tectonic cycles taken place in the period of the Jurassic and the Early Cretaceous, respectively. Then it is obtained the following conclusion that the mountains has lost its tectonic affinity of the craton since the late of the early Cretaceous and changed into part of a composite orogenic region which is composed by the western margin of the East Asian orogenic region and the southern part of the North Asian orogenic one. In the same time, it is the first time to publish some new data on structural deformation from those three units and put forward to some new viewpoints on the mountains i.e. that the the present geomorphological features of the mountains occurs in the late of the Cenozoic, that the area underwent four periods of crustal shortening events in the end of the Early Paleozoic, the latest of the Paleozoic, the late of the Jurassic and the late of the Early Cretaceous, respectively, that the central unit may be sub−divided into four sub−belts, that the three stages of structural deformation of Bayan Obo group sedimentary sequences are distinguishied into tight folding in the early one, and then the right−side strike−slip in the second, and northward thrusting in the third, and that the the timing of the intensely north−verging thrusting of the south unit is determined as the late of the Early Cretaceous. Lastly, some suggestions on the tectonic issue which remain to be further studied and investigated in the mountains, are briefly stated.
-
Keywords:
- Yinshan mountains /
- craton /
- accreted orogen /
- activated orogen /
- orogenic region
-
-
![]()
图 1 阴山山脉地貌特征（所用数字高程数据为NASA提供的SRTM GTOPO 30格式，据网址http://glcf.umiacs.umd.edu）
Figure 1. DEM of Yinshan mountains, showing its geomorphologic feartues
![]()
图 2 阴山山脉区域地质构造背景（据李锦轶等，2014修改）
实线—造山区与克拉通的界线（褐色为北亚造山区的边界，粉色为南亚造山区的北界，绿色为东亚造山区的西界）；双断线—古板块缝合带（褐色为古生代晚期，蓝色为三叠纪晚期，绿色为侏罗纪晚期，红色为新生代）；蓝色断线—扬子古克拉通的东南边界；NCC—古华北克拉通；YZC—古扬子克拉通；QDSL—秦岭-大别-苏鲁造山带
Figure 2. Regional geological settings of Yinshan mountains
![]()
图 3 阴山山脉南部地貌地质构造及其与中生代推覆构造的空间关系
Figure 3. Geomorphological map of southern Yinshan mountains, showing the Cenozoic faults and its relation to Mesozoic nappe structures
![]()
图 4 阴山山脉地质构造简图（底图据李仰春等, 2020）
Figure 4. Simplified geological map of Yinshan mountains
![]()
图 7 前根达来混杂岩野外露头和主要地质现象（拍摄自百灵庙镇以北露头区）
Figure 7. Field pictures of the bird-view and main geological features of the Qiangendalai mélange
![]()
图 8 百灵庙镇以北地区早古生代浅变质岩中的紧闭同斜褶皱
Figure 8. Field pictures taking in the north of Bailingmiao town, showing the southeastwards tight pinched recumbent fold of the Early Paleozoic (possiblly the Siliurian) metasedimentary sequences
![]()
图 9 乌德以南地区晚志留世—泥盆纪滑塌堆积露头景观(A)和探槽(B)照片
Figure 9. Pictures of the outcrop(A) and artificial section(B) of the Late Silurian to Devonian olistolith taking from the south to Wude herd
![]()
图 10 乌德-白乃庙断裂西段构造变形特征野外照片
Figure 10. The tectonic deformation field pictures from the western segmemt of Wude-Bailingmiao fault
![]()
图 11 百灵庙镇西郊白云鄂博群构造变形特征（照片上红色线条为断层，绿色线条为构造面理，每个照片所显示的构造现象详见正文）
Figure 11. Field pictures taking from the west of Bailingmiao town, showing the feature of structural deformation of the Baiyunebo group
![]()
图 12 百灵庙镇西北被置于寒武纪沉积岩系构造变形（绿色线条为突出表示的沉积层理褶皱）
Figure 12. Field picture taking from the outcrop northwest of Bailingmiao town, showing the structural deformation of the supposed Cambrian sedimentary strata
![]()
图 13 白云鄂博群构造变形的宏观特征
Figure 13. The feartue of outcrops and structural deformation of the Baiyunebo group
![]()
图 14 阴山山脉西端海流图镇西北地区可能的侏罗纪 推覆构造
Figure 14. Supposed latest Jurassic nappe structure in the northwest Hailiutu town
![]()
图 16 固阳北东巨宝庄逆冲叠瓦构造
Figure 16. Jubaozhuang imbricated thrusting structure in northeast to Guyang county
![]()
图 17 阴山山脉南缘色尔腾山地质构造简图
Figure 17. Simplified geological and tectonic map of Seertengshan in southern margin of Yinshan mountains
-
Bai X H, Xu Z Y, Liu Z H, et al. 2015. Zircon U−Pb dating, geochemistry and geological significance of the Early Silurian plutons from the southeastern margin of the Central Asian Orogenic Belt[J]. Acta Petrologica Sinica, 31(1): 67−79( in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Inner Mongolian Autonomous Region. 1991. Regional Geology of Inner Mongolian Autonomous Region[M]. Beijing: Geological Publishing House, 1−725 (in Chinese).
Burg J P, Ford M. 1997. Orogeny through time: an overview[C]// Burg J P, Ford M. Orogeny Through Time. Geological Society Special Publication, 121: 1−17.
Cawood P A, Hawkesworth C J, Dhuime B. 2013. The continental record and the generation of continental crust[J]. GSA Bull., 125: 14−32. doi: 10.1130/B30722.1
Chen Q, Qiu G L, Du Y Z, et al. 1992. Regionl tectonics of Bainaimiao−Wenduermiao area and Paleo−plate tectonic evolution of the northern margin of North China[J]. Bulletin of Changchun Institute of Geology, (22): 119−129(in Chinese with English abstract).
Chen Z Y, Wen C S, Zhang W J. 2000. Nappe structure in mount Seerteng, Inner Mongolia[J]. Earth Sciences, 25(3): 237−282(in Chinese with English abstract).
Chen Z Y, Li Y X, Wang X L et al. 2002. Thrust nappe structure in the Bap−northern Hohhot area, Inner Mongolia[J]. Geological Bulletin of China, 21(4/5): 251−258(in Chinese with English abstract).
Cheng S P, Deng Q D, Yang G Z, et al. 2000. On the Cenozoic denudation and uplift of fhe Daqingshan mountains, Inner Mongolia[J]. Seismology and Geology, 22(1): 27−36(in Chinese with English abstract).
Chu H, Zhang J R, Wei C J, et al. 2013. A new interpretation of the tectonic setting and age of meta−basic volcanics in the Ondor Sum Group, Inner Mongolia[J]. Chin. Sci. Bull., 58: 3580−3587. doi: 10.1007/s11434-013-5862-7
Dang Z C, Li J J, Zhao Z L, et al. 2016. LA−ICP−MS zircon U−Pb dating of the gabbro from Xiaonanshan, Siziwang Banner, Inner Mongolia, and its geological significance[J]. Geological Bulletin of China, 35(4): 583−592(in Chinese with English abstract).
Dang Z C, Li J J, Fu C, et al. 2018. Geochronological, mineralogical and lithogeochemical studies of the Kebu mafic−ultramafic intrusion in Urad Middle Banner, Inner Mongolia[J]. Acta Geologica Sinica, 92(2): 278−297(in Chinese with English abstract).
Darby B J. 1999. Structutal evolutiom of the southweitern Daqingshan, Yinshan belt, Inner Mongolia, Chima[D]. Master Thesis, University of Southern California, Los Angeles.
Davis G A, Wang C, Zheng Y D, et al. 1998. The enigmatic Yinshan fold−and –thrust belt of northern China: New views on its intraplate contractional styles[J]. Geology, 26: 43−46.
Davis G A, Zheng Y D, Wang C, et al. 2001. Mesozoic tectonic evolution of the Yanshan fold and thrust belt, with emphasis on Hebei and Liaoning provinces, Northern China[J]. Geological Society of America Memoir, 2001: 171–197.
Davis G A, Darby J B, Zheng Y D, et al. 2002. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex, Inner Mongolia, China[J]. Geology, 30(11): 1003−1006. doi: 10.1130/0091-7613(2002)030<1003:GATEOA>2.0.CO;2
Davis G A, Darby B J. 2010. Early Cretaceous overprinting of the Mesozoic Daqing Shan fold and thrust belt by the Hohhot metamorphic core complex, Inner Mongolia, China[J]. Geoscience Frontiers, 1(1): 1−20. doi: 10.1016/j.gsf.2010.08.001
Dewey J F, Horsfield B. 1970. Plate tectonics, orogeny and continental growth[J]. Nature, 225: 521−525. doi: 10.1038/225521a0
De Jong K, Xiao W J, Windley B F, et al. 2006. Ordovician 40Ar/39Ar phengite ages from the blueschist−facies Ondor Sum subduction−accretion complex (Inner Mongolia) and implications for the early Paleozoic history of continental blocks in China and adjacent areas[J]. American Journal of Science, 306: 799−845. doi: 10.2475/10.2006.02
De Wit M J, Roering C, Hart R J, et al. 1992. Formation of an Archaean continent[J]. Nature, 357: 553−56. doi: 10.1038/357553a0
Dong C Y, Ma M Z , Xie H Q, et al. 2021. Magmatism and metamorphism of the Early Precambrian basement in the Bayan Obo area, Inner Mongolia: Zircon SHRIMP U−Pb dating and LA−MC−ICPMS Hf analysis[J]. Acta Petrologica Sinica, 37(2): 417−432(in Chinese with English abstract).
Du J M, Zhang Q L, Xu S Y, et al. 2009. Characters of later Jurassic Yinshan intraplate orogeny belt: Evidence from Daqing Shan, Inner Mongolia[J]. Acta Geologica Sinica, 83(7): 910−922(in Chinese with English abstract).
Fan H R, Hu F F, Chen F K, et al. 2006. Intrusive age of No. 1 carbonatite dyke from Bayan Obo REE−Nb−Fe deposit, Inner Mongolia: with answers to comment of Dr. Le Bas[J]. Acta Petrologica Sinica, 22(2): 519−520(in Chinese with English abstract).
Fan H R, Hu F F, Yang K F, et al. 2009. Geochronology framework of late Paleozoic dioritic−ganitic pluton in the Bayan Obo area, Inner Mongolia, and tectonic significance[J]. Acta Petrologica Sinica, 25(11): 2933−2938(in Chinese with English abstract).
Fan H R, Yang K F, Hu F F, et al. 2010. Zircon geochronology of basement rocks from the Bayan Obo area, Inner Mongolia, and tectonic implications[J]. Acta Petrologica Sinica, 26(5): 1342−1350(in Chinese with English abstract).
Feng S Y, Liu B J, Ji J F. 2015. The survey on fine lithospheric structure beneath Hohhot Baotou basin by deep seismic reflection profile[J]. Chinese J. Geophysics, 58(4): 1158−1168 (in Chinese with English abstract).
Feng F, Xu Z Y, Dong X J, et al. 2021. Chronology, geochemistry and Hf isotope of granite porphyry in Wenduermiao−Jining area, Inner Mongolia[J]. Earth Science, 46(6): 1973−1992 (in Chinese with English abstract).
Feng L X, Zhang Z C, Han B F, et al. 2013. LA−ICP−MS zircon U−Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia, and their geological significance[J]. Geological Bulletin of China, 32(11): 1737−1748(in Chinese with English abstract).
Gao D Z, Li L, Zhang W J. 2001. Tectonic characterisitics and evolution of the central segment of the Linhe−Jining fault belt, Inner Mongolia[J]. Regional Geology of China, 20(4): 337−342(in Chinese with English abstract).
Ge X H. 1989. The history of formation of intraplate orogenic belts in the North China paleoplate[J]. Geological Review, 35(3): 254−262(in Chinese with English abstract).
GEO/EAR (the Tectonics Program, Earth Sciences Division, and National Science Foundation). 2003. New Departures in Structural Geology and Tectonics[C]. 1−61. http://www.pangea.stanford.edu/~dpollard/NSF/.
Gong M, Cai J H, Yan G H, et al. 2019. Petrogeochemical characteristics and zircon SHRIMP U−Pb ages of the alkaline intrusions on northern side of the Yinshan Mountains−Yanshan Mountains and their tectonic significances[J]. Geological Review, 65(4): 894−913(in Chinese with English abstract).
Guo L, Wang T, Castro A, et al. 2012a. Petrogenesis and evolution of Late Mesozoic granitic magmatism in the Hohhot metamorphic core complex, Daqing Shan, North China[J]. International Geology Review, 54(16): 1885−1905.
Guo L, Wang T, Zhang J J, et al. 2012. Evolution and time of formation of the Hohhot metamorphic core complex, North China: New structural and geochronological evidence[J]. International Geology Review 54(11): 1309–1331.
Hao B W, Jiang J. 2010. Chronology, geochemistry of the Hadamiao complex related to gold deposits in Xianghuang Banner, Inner Mongolia[J]. Acta Petrologica et Mineralogica, 29(6): 750−762(in Chinese with English abstract).
He Z J, Li J Y, Niu B G, et al. 1998. A late Jurassic intese thrusting−uplifting event in the Yanshan−Yinshan area, Northern China, and its sedimentary response[J]. Geological Review, 44(4): 407−418(in Chinese with English abstract).
He Z J, Wang Z Q, Ren J S. 1999. Primary investigations on the features and origin of sedimentary basins in front of the Jurassic large−scale nappe in the northern region of North China[J]. Scientia Geologica Sinica, 34(2): 186−195(in Chinese with English abstract).
Holdsworth R E, Hand L M, Miller J A, et al. 2001. Continental reactivation and reworking: An introduction[J]. Geol. Soc. Spec. Publ., 184: 1−12. doi: 10.1144/GSL.SP.2001.184.01.01
Hou J G, Su S G, Zhou D, et al. 2014. Petrological and geochemical characteristics of basic−ultrabasic complex from southern Wengen in Inner Mongolia and its tectonic setting[J]. Acta Petrologica Sinica, 30(12): 3729−3740 (in Chinese with English abstract).
Hu X. 1983. Glaucophane schists and their geological nature in Inner Mongolia[C]//Contributions to the Project of Plate Tectonics in Morthern China, Shenyang. Shenyang Institute of Geology and Mineral Resources: 230−242(in Chinese with English abstract).
Hu X. 1985. The subduction speed and depth of the early Paleozoic Wenduermiao plate subduction zone in the east Inner Mongolia[J]. Bulletin of Hebei College of Geology, (4): 33−40 (in Chinese with English abstract).
Hu X, Niu S Y. 1992. Structural deformation and evolution of the Mid−Proterozoic in the Langshan and Zhaertaishan, Inner Mongolia[J]. Regional Geology of China, (1): 75−82(in Chinese with English abstract).
Hu X, Xu C S, Niu S Y. 1990. Evolution of the Early Paleozoic Continental Margin of North China platform[M]. Beijing: Peking University Publishing House: 1−215 (in Chinese).
Hu X J, Yang Z L, Wang S Q, et al. 2022. Geochronology and geochemistry of the Early Paleozoic volcanic rocks from the Baoerhantu arc in Inner Mongolia: petrogenesis and constraints on the tectonic evolution of the Xing−Meng orogenic belt[J]. Acta Geologica Sinica, 96(3): 897−917 (in Chinese with English abstract).
Huang D L, Hou Q Y. 2017. Devonian alkaline magmatism in the northern North China Craton: geochemistry, SHRIMP zircon U−Pb geochronology and Sr−Nd−Hf isotopes[J]. Geoscience Frontiers, 8(1): 171−181. doi: 10.1016/j.gsf.2016.02.006
Huang T K. 1945. On Major Tectonic Forms of China[M]. Geol. Momoirs, Ser A, 20: 1−165.
Huang T K. 1960. Primary summary of major features of tectonics of China[J]. Acta Geologica Sinica, 40(1): 1−32(in Chinese).
Huang T K. Ren J S, Jiang C F, et al. 1977. An outline of the tectonic characteristics of China[J]. Acta Geologica Sinica, (2): 117−135(in Chinese with English abstract).
Huang T K. 1979. On some of the tectonic characteristics of China, with special discussion on the polycyclic development of geosynclinals foldbelts[J]. Acta Geologica Sinica, (2): 99−111(in Chinese with English abstract).
Huang T K. 1984. New researches on the tectonic characteristics of China[J]. Bulletin of the Chinese Academy of Geological Sciences, 9: 4−18(in Chinese with English abstract).
Huntington K W, Klepeis K A, Allmendinger R, et al. 2018. Challenges and opportunities for research in tectonics: Understanding deformation and the processes that link Earth systems, from geologic time to human time. A community vision document submitted to the U. S. National Science Foundation[M]. University of Washington: 1−84.
Isozaki Y. 1997. Contrasting two types of orogen in Permo−Triassic Japan: Accretionary versus collisional[J]. Island Arc, 6(1): 2−24. doi: 10.1111/j.1440-1738.1997.tb00038.x
Jia B W, Wu Y Q. 1995. The provenance and stratigraphic significance of volcanic event layers in late Paleozoic coal measures from Daqingshan, Inner Mongolia[J]. Journal of Geology and Mineral Resources of North China, 10(2): 203−213(in Chinese with English abstract).
Jia H Y, Baoyinwuliji, Zhang Y Q. 2003. Characteristics and tectonic significance of the wude suture zone in northern Damaoqi, Inner Mongolia[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 30(1): 30−34(in Chinese with English abstract).
Jahn B M. 2004. The Central Asian orogenic belt and growth of the continental crust in the Phanerozoic [C]//Malpas J. Aspects of the tectonic evolution of China. Geological Society, London, Special Publications, 226: 73−100.
Jiang N. 2005. Petrology and geochemistry of the Shuiquangou syenitic complex, northern margin of the North China Craton[J]. Journal of the Geological Society, 162(1): 203−215. doi: 10.1144/0016-764903-144
Jin S K, Liu B, Ma M, et al. 2024. Zircon U−Pb geochronology, geochemistry, and Sr−Nd−Hf isotopic characteristics of the Permian−Triassic granitic intrusions in the Huade area, Inner Mongolia, NE China: Constraints on the tectonic evolution of the Paleo−Asian Ocean[J]. Acta Geologica Sinica, 98(1): 116−137(in Chinese with English abstract).
Johnson M E, Rong J Y, Wang C Y, et al. 2001. Continental island from the Upper Silurian (Ludfordian Stage) of Inner Mongolia: Implications for eustasy and paleogeography[J]. Geology, 29(10): 955−958.
Kang Y Z. 2007. The main tectonic systems and their controls on petroleum resource in China[J]. West China Petroleum Geosciences, 3(1): 1−8(in Chinese with English abstract).
Law R D, Butler R W H, Holdsworth R E, et al. 2010. Continental tectonics and mountain building. The Legacy of Peach and Horne: An Introduction[J]. Geol. Soc. Spec. Publ., 335: 1−6. doi: 10.1144/SP335.1
Lee C T, Luffi P, Chin E J. 2011. Building and destroying continental mantle[J]. Annu. Rev. Earth Planet Sci., 39: 59−90. doi: 10.1146/annurev-earth-040610-133505
Le Bas M J. 2006. Re−interpretation of zircon date in a carbonatite dyke at the Bayan Obo giant REE−Fe−Nb deposit, China[J]. Acta Petrologica Sinica, 22(2): 517−518.
Leng Y B, Zhang Y H, Chen Y J, et al. 2019. Characteristics and significance of metabasalt in Zhurihe area, central Inner Mongolia[J]. Global Geology, 3(3): 598−610(in Chinese with English abstract).
Li C D, Ran H, Zhao L G, et al. 2012. LA−MC−ICPMS U−Pb geochronology of zircons from the Wenduermiao group and its tectonic significance[J]. Acts Petrologica Sinica, 28(11): 3705−3714(in Chinese with English abstract).
Li C Y, Wang Q, Liu X Y, et al. 1982. Tectonic Map of Asia (1: 8, 000, 000) and Its Explanatory Notes [M]. Beijing: SinoMaps Press (in Chinese).
Li C Y, Tang Y Q. 1983. Some problems on subdivision of paleo−plate in Asia[J]. Acta Geologica Sinica, 57(1): 1−10(in Chinese with English abstract).
Li G, Liu Z H, Xu Z Y, et al. 2012. Components of the Bainaimiao thrust and its structural features[J]. Journal of Jilin in University (Earth Science Edition), 42(1): 309−319 (in Chinese with English abstract).
Li J F, Zhang Z C, Han B F. 2020. Ar−Ar and zircon SHRIMP geochronology of hornblendite and diorite in northern Darhan Muminggan Joint Banner, Inner Mongolia, and its geological significance[J]. Acta Petrologica et Mineralogica, 29(6): 732−740(in Chinese with English abstract).
Li J J, Dang Z C, Zhao Z L. 2015. The meta ogenic epochs of Bainaimiao group copper deposit in Inner Mongolia[J]. Acta Geologica Sinica, 89(8): 1448−1457(in Chinese with English abstract).
Li J L, Hu F Y. 1981. The serpentinitic olistostrome in Bayanobo group[J]. Scientia Geologica Sinica, 16(3): 269−273(in Chinese with English abstract).
Li J Y. 2006. Permian geodynamic setting of Northeast China and adjacent regions: Closure of the Paleo−Asian Ocean and subduction of the Paleo−Pacific Plate[J]. Journal of Asian Earth Sciences, 26(3/4): 207−224.
Li J Y. 2009. Cycles and Stages of Geological History of China Mainland[J]. Geology in China, 36(3): 504−521(in Chinese with English abstract).
Li J Y, He G Q, Xu X, et al. 2006. Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation[J]. Acta Geologica Sinica, 80(1): 148−168(in Chinese with English abstract).
Li J Y, Gao L M, Sun G H, et al. 2007. Shuangjingzi middleTriassic syn−collisional crust−derived granite in the east Inner Mongolia and its constraint on the timing of collision between Siberian and Sino−Korean paleo−plates[J]. Acta Petrologica Sinica, 23(3): 565−582(in Chinese with English abstract).
Li J Y, Zhang J, Yang T N. 2009. Crustal tectonic division and evolution of the southern part of the North Asian Orogenic Region and its adjacent areas[J]. Journal of Jilin University(Earth Science Edition), 39(4): 584−605(in Chinese with English abstract).
Li J Y, Zhang J, Liu J F, et al. 2014. Major deformation systems in the mainland of China[J]. Earth Science Frontiers, 21(3); 226−245(in Chinese with English abstract).
Li J Y, Liu J F, Qu J F, et al. 2019a. Major geological features and crustal tectonic framework of Northeast China[J]. Acta Petrologica Sinica, 35(10): 2989−3016(in Chinese with English abstract). doi: 10.18654/1000-0569/2019.10.04
Li J Y, Zhang J, Liu J F, et al. 2019b. Crustal tectonic framework of China and its formation processes: constraints from structural deformation[J]. Journal of Geomechanics, 25(5): 678−698(in Chinese with English abstract).
Li W B, Hu C S, Zhong R C, et al. 2015. U−Pb, 39Ar/40Ar geochronology of the metamorphosed volcanic rocks of the Bainaimiao Group in central Inner Mongolia and its implications for oregenesis and geodynamic setting[J]. Journal of Asian Earth Sciences, 97: 251−259. doi: 10.1016/j.jseaes.2014.06.007
Li S Q, Chen Y J, Han R D, et al. 2017. Chronology and geochemistry of meta−basic volcanics of Baiyinnuoer region in Wenduermiao area, Inner Mongolia[J]. Global Geology, 36(2): 428−440(in Chinese with English abstract).
Li W B, Chen Y J, Lai Y, et al. 2008. Metallogenic time and tectonic setting of the Bainaimiao Cu−Au deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 24(4): 890−898 (in Chinese with English abstract).
Li W B, Zhong R C, Xu C, et al. 2012. U−Pb and Re−Os geochronology of the Bainaimiao Cu−Mo−Au deposit, on the northern Margin of the North China Craton, Central Asia Orogenic Belt: Implications for oregenesis and geodynamic setting[J]. Ore Geology Reviews, 48: 139−150. doi: 10.1016/j.oregeorev.2012.03.001
Li Y C, Li Z P, Gu Y C, et al. 2020. Geological Map of China with a scale of 1;1500000[M]. Beijing: Geological Publishing House (in Chinese).
Li Y X, Hu F X, Chen Z Y, et al. 2002. Extensional structure in the Shenshuiliang area in the northern part of Qixiaying, Inner Mongolia[J]. Geological Bulletin of China, 21(4/5): 259−263(in Chinese with English abstract).
Liu C F, Yang S S, Wu J W, et al. 2010. Dating and petrogenesis of Late Permian−early Triassic peraluminous granites in the Siziwangqi area, Inner Mongolia[J]. Acta Geologica Sinica, 84(5): 1012−1016(in Chinese with English abstract).
Liu C F, Liu W C, Zhou Z G. 2014a. Geochronology, Geochemistry and Tectonic Setting of the Paleozoic−EarlyMesozoic Intrusive in Siziwangqi, Inner Mongolia[J]. Acta Geologica Sinica, 88(6): 992−1002(in Chinese with English abstract).
Liu C F. Ltu W C, Wang H P, et al. 2014b. Geochronology and in the geochemistry of the Bainaimiao metavolcanic rocks in the northern margin of North China Craton[J]. Acta Geologica Sinica, 88(7): 1273−1287(in Chinese with English abstract).
Liu D Y, Jian P, Zhang Q, et al. 2003. SHRIMP dating of adalites in the Tulingkai ophiolite, Inner Mongolia: Evidence for the early Paleozoic subduction[J]. Acta Geologica Sinica, 77(3): 317−327 (in Chinese with English abstract).
Liu J, Zhang J J, Guo L, et al. 2014. 40Ar−39Ar dating of the detachment fault of the Hohhot metamorphic core complex, Inner Mongolia, China[J]. Acta Petrologica Sinica, 30(7): 1899−1908(in Chinese with English abstract).
Liu J F, Li J Y, Chi X G, et al. 2013. Zircon U−Pb dating and geochemistry of the Early Devonian volcanic rocks related to arc−continent collision in the northern margin of North China craton[J]. Geological Bullletin of China, 32 (2/3): 267−278(in Chinese with English abstract).
Liu J M, Zhao Y, Sun L L, et al. 2010. Recognition of the latest Permian to Early Triassic Cu−Mo mineralization on the northern margin of the North China block and its geological significance[J]. Gondwana Res., 17: 125−134. doi: 10.1016/j.gr.2009.07.007
Liu L S, Gao L, Du A D, et al. 1996. The Re−Os isotopic age of molybdenite from Bayan Obo REE ore deposit[J]. Mineral Deposits, 15(2): 188−191(in Chinese with English abstract).
Liu Y L, Yang G, Chen J F, et al. 2005. Pyrite Re−Os dating of Bayan Obo REE−Nb−Fe ore deposit[J]. Chinese Science Bulletin, 50(2): 172−175(in Chinese).
Liu Z H, Xu Z Y, Yang Z S. 1999. The thrusting tectonics in Daqingshan, Inner Mongolia[J]. Regional Geology of China, 18(4): 366−372(in Chinese with English abstract).
Liu Z H, Xu Z Y, Yang Z S. 2001. Daqingshan thrust system signification and its geological characteristics[J]. World Geology, 20(3): 223−230(in Chinese with English abstract).
Liu Z H, Xu Z Y, Yang Z S. 2002. Mesozoic crustal overthrusting and extensional deformation in the Yinshan mountains area[J]. Geological Bulletin of China, 21(4/5): 246−230(in Chinese with English abstract).
Liu Z H, Xu Z Y, Yang Z S. 2003a. 40Ar−39Ar dating of Daqingshan thrust[J]. Chinese Science Bulletin, 48(24): 2734−2738.
Liu Z H, Xu Z Y, Yang Z S. 2003b. Indosinian tectonic movement in the Daqingshan region in Inner Mongolia[J]. Geological Review, 49(5): 457−463(in Chinese with English abstract).
Lu J S, Ni Z Y, Zhai M G, et al. 2009. Petrology and geochemistry of the metamorphic peridotites within the Hongqiyingzi group in Chicheng, north Hebei provinve, China[J]. Journal of Mineral and Petrology, 29(3): 91−99(in Chinese with English abstract).
Lu Y H, Li W B, Lai Y. 2009. Time and tectonic setting of hosting porphyry of the Hadamiao gold deposit in Xianghuangqi, Inner Mongolia[J]. Acta Petrologica Sinica, 25(10): 2615−2620(in Chinese with English abstract).
Luo H L, Wu T R, Li Y. 2007. Geochemistry and SHRIMP dating of the Kebu massif from Wulatezhongqi, Inner Mongolia: Evidence for the Early Permian underplating beneath the North China Craton[J]. Acta Petrologica Sinica, 23(4): 755−76(in Chinese with English abstract).
Luo H L, Wu T R, Zhao L. 2009. Zircon SHRIMP U−Pb dating of Wuliangsitai A−type granite on the northern margin of the North China plate and tectonic significance[J]. Acta Petrologica Sinica, 25(3): 515−526(in Chinese with English abstract).
Luo Z K, Miao L C, Guan K, et al. 2001. SHRIMP chronological study of Shuiquangou intrusive body in Zhangjiakou area, Hebei province and its geochemical significance[J]. Geochimica, 30(2): 116−122(in Chinese with English abstract).
Lv Z, Wang J P, Wang J C, et al. 2022. Geochronology and geological significance of intrusive rocks in the Bainaimiao Cu−Au deposit, Inner Mongolia[J]. Geoscience, 36(1): 307−319(in Chinese with English abstract).
Ma G, Shen P, Pan H, et al. 2019. Zircon U−Pb geochronology, trace element composition and geochemistry of ore−bearing porphyry in Bainaimiao Cu−Au deposit, Inner Mongolia, and the implications for mineralization[J]. Acta Geologica Sinica, 93(12): 3144−3165 (in Chinese with English abstract).
Ma Y F, Jiao J G, Guo T M, et al. 2022. Petrogenesis and mineralization potentials of mafic−ultramafic intrusions in the Xiaonanshan region, Siziwangqi, Inner Mongolia[J]. Acta Geologica Sinica, 96(12): 4312−4330 (in Chinese with English abstract).
Miao L C, Qiu Y M, Guan K, et al. 2001a. A Chronological study of SHRIMP U−Pb of zircon from the Dahuabei intrusion in the Wulashan area, Inner Mongolia[J]. Geological Review, 47(2): 169−173(in Chinese with English abstract).
Miao L C, Zhai Y S, Zhu C W, et al. 2001b. Study on chronology of the Shuiquangou alkali complex in northwestern Hebei province, P. R. China[J]. Gold Geology, 7(1): 1−6(in Chinese with English abstract).
Miyashiro A, Aki K, Sengor A M C. 1982. Orogeny[M]. John Wiley & Sons Ltd. : 1−236.
Molnar P. 1988. Continental tectonics in the aftermath of plate tectonics[J]. Nature, 335: 131−137. doi: 10.1038/335131a0
Nie F J, Pei R F, Wu L S, et al. 1995. Nd− and Sr−istope study on the greenschist and granodiorite of the Bainaimiao district, Inner Mongolia, China[J]. Acta Geoscientia Sinica, (1): 36−44 (in Chinese with English abstract).
Ni Z Y, Zhai M G, Wang R M, et al. 2006. Late Paleozoic retrograded eclogites from within the northern margin of the North China Craton: Evidence for subduction of the Paleo−Asian ocean[J]. Gondwana Research, 9: 209−224. doi: 10.1016/j.gr.2005.06.014
Parfenov L M, Popeko L I, Tomurtogoo O. 2001. Problems of tectonics of the Mongol–Okhotsk orogenic belt[J]. Geology of the Pacific Ocean, 16: 797−830.
Peng L H. 1984. Geological ages of south ophiolite belt in Wenduermiao group, Inner Mongolia and its tectonic significance[J]. Chinese Science Bulletin, 29(2): 104−107(in Chinese).
Phinney R A, Silver P, Lerner−Lam A, et al. 1989. A National Program for Research in Continental Dynamics [R]. A report to National Science Foundation, U. S. Geological Survey, and U. S. Deparment of Energy: 1−72.
Qi G W, Zhang J J, Wang X S, et al. 2007. Mesozoic thrusts and extensional structures in the Daqingshan orogen, Inner Mongolia, and their temporal and spatial relationship[J]. Progress in Natural Science, 17(2): 177−186 (in Chinese with English abstract).
Qi S J, Hu X, Ding F Q, et al. 1979. Evidence of Ancient plate movement of Inner Mongolia and its relationship with geosynclinals evolution[J]. Bulletin of Hebei College of Geology, (3): 1−13 (in Chinese with English abstract).
Qiao X F, Gao L Z, Peng Y, et al. 1997. Composite stratigraphy of the Sinlinhuodong group and ore−bearing micrite mound in the Bayan Obo deposit, Inner Mongolia, China[J]. Acta Geologica Sinica, 71(3): 202−211(in Chinese with English abstract).
Qin Y, Liang Y H, Xing J L, et al. 2013. The identification of Early Paleozoic adakitic rocks in Zhengxiangbaiqi area , inner Mongolia and its significance[J]. Earth Science Frontiers, 20(5): 106−114(in Chinese with English abstract).
Ren J S, Wang Z X, Chen B W, et al. 1999. The Tectonics of China From a Global View––A Guide to the Tectonic Map of China and Adjacent Regions[M]. Beijing: Geological Publishing House (in Chinese).
Ren Y C, Zhang Y C, Zhang Z Q. 1994. Study of heat events of ore−forming Bayan Obo Deposit[J]. Acta Geoscientia Sinica, (Z1): 95−101 (in Chinese with English abstract).
Ritts B D, Darby B J, Cope T. 2001. Early Jurassic extensional basin formation in the Daqing Shan segment of the Yinshan belt, northern North China Block, Inner Mongolia[J]. Tectonophysics, 339: 239−258. doi: 10.1016/S0040-1951(01)00115-9
Rong J Y, Johnson M E, Baarli B G, et al. 2001. Continental island from the Upper Silurian (Ludlow) Sino-Korean plate[J]. Chinese Science Bulletin, 46: 238−241.
Rudnick R L, Gao S. 2003. Composition of the continental crust[J]. Treatise on Geochemistry, 3: 1−64.
Ryan P D, Mac Niocaill C. 1999. Continental tectonics: An introduction[J]. Geol. Soc. Spec. Publ., 164: 1−5. doi: 10.1144/GSL.SP.1999.164.01.02
Şengör A M C. 1990. Plate tectonics and orogenic research after 25 years: A Tethyan perspective[J]. Earth Science Reviews, 27: 1−201. doi: 10.1016/0012-8252(90)90002-D
Shang H S, Tao J X, Baoyinwuliji, et al. 2003. The arc−basin System and tectonic significance of Early Paleozoic in Baiyun’ebo area, Inner Mongolia[J]. Geological Survey and Research, 26(3): 160−168(in Chinese with English abstract).
Shao J A. 1991. Crust Evolution in the Middle Part of the Northern Margin of Sino−Korean Plate[M]. Beijing: Peking University Publishing House: 1−136(in Chinese with English abstract).
Shi Y R, Liu D Y, Miao L C, et al. 2010. Devonian A−type granitic magmatism on the northern margin of the North China Craton: SHRIMP U−Pb zircon dating and Hf−isotopes of the Hongshan granite at Chifeng, Inner Mongolia, China[J]. Gondwana Research, 17(4): 632−641. doi: 10.1016/j.gr.2009.11.011
Sleep N H. 2005. Evolution of the continental lithosphere[J]. Annu. Rev. Earth Planet Sci., 33: 369−393. doi: 10.1146/annurev.earth.33.092203.122643
Su W B, Li W G, Li H M, et al. 2022. SHRIMP Zircon U−Pb geochronology of the tuffite layer in the Shinagan group, Inner Mongolia, North China Craton[J]. North China Geology, 45(2): 51−67(in Chinese with English abstract).
Su Y Z, Tang K D, Chi Y Y, et al. 1983. A new section of Upper Silurian Xibiehe formation in northeast of Bayan Obo, Inner Mongolia[C]//Contributions to the Project of Plate Tectonics in Morthern China. Shenyang: Shenyang Institute of Geology and Mineral Resources: 221−229(in Chinese with English abstract).
Sun L X, Ren B F, Teng F, et al. 2015. LA−ICP−MS zircon U−Pb ages of the volcanoic rocks from the Chaotugou Formation in Aohan Banner, Inner Mongolia. Geological Bulletin of China, 34(8): 1493−1501(in Chinese with English abstract).
Sun L X, Zhang Y, Li Y, et al. 2017. Geochemical characteristics and intraplate extension of Late Devonian bimodal volcanic rocks in Chifeng area of Inner Mongolia[J]. Geology in China, 44(2): 371−388(in Chinese with English abstract).
Tang K. 1990. Tectonic development of Palaeozoic fold belts at the north margin of the Sino−Korean craton[J]. Tectonics, 9: 249−260. doi: 10.1029/TC009i002p00249
Tang K D, et al. 1992. Tectonic Evolution and Mineragenetic Regularities of the Fold Belt along the Northern Margins of Sino−Korean Plate[M]. Beijing: Peking University Publishing House: 1−277(in Chinese with English abstract).
Tang K, Yan Z. 1993. Regional metamorphism and tectonic evolution of the Inner Mongolian suture zone[J]. Journal of Metamorphic Geology, 11: 511−522. doi: 10.1111/j.1525-1314.1993.tb00168.x
Tang K D, Yan Z Y, Zhang Y P. et al. 1983. On Wenduermiao group and its tectonic significance[C]//Contributions to the Project of Plate Tectonics in Morthern China. Shenyang: Shenyang Institute of Geology and Mineral Resources: 186−205(in Chinese with English abstract).
Teng X M, Yang Q Y, Santosh M. 2015. Devonian magmatism associated with arc−continent collision in the northern North China Craton: Evidence from the Longwangmiao ultramafic intrusion in the Damiao area[J]. Journal of Asian Earth Sciences, 113: 626−643. doi: 10.1016/j.jseaes.2015.04.032
Tian T, Ni Z Y, Pan D, et al. 2018. Late Paleozoic granites within Kangbao area, north Hebei province: Zircon U−Pb dating and tectonic implications[J]. Chinese Journal of Geology, 53(2): 661−667(in Chinese with English abstract).
Wakita K. 2001. Comparison of Two Types of Orogenic Belts − Collision vs. Accretion[J]. Gondwana Research, 4(4): 811. doi: 10.1016/S1342-937X(05)70597-9
Wang B, Shi L Z, Yuan Z, et al. 2022. Geochemistry and significance of siliciclastic rocks from the lowest Elitu formation of Middle Permian in the Gongnaoer area, Zhengxiangbaiqi, Inner Mongolia[J]. Acta Geoscientica Sinica, 43(4): 569−583 (in Chinese with English abstract).
Wang F, Chen F K, Siebel W, et al. 2011. Zircon U–Pb geochronology and Hf isotopic composition of the Hongqiyingzi Complex, northern Hebei Province: New evidence for Paleoproterozoic and late Paleozoic evolution of the northern margin of the North China Craton[J]. Gondwana Research, 20: 122−136. doi: 10.1016/j.gr.2011.02.003
Wang H C, Yuan G B, Xin H T, 1999. On the tectonic implication for Xiashihao−Jiuguan ductile shear zone in Guyang−Wuchuan area, Inner Mongolia[J]. Progress in Precambrian Research, 22(1): 12−20 (in Chinese with English abstract).
Wang H C, Chu H, Xiang Z Q, et al. 2012a. The Hongqiyingzi group in the Chongli−Chicheng area, northern margin of the North China craton: A suite of late Paleozoic metamorphic complex[J]. Earth Science Frontiers, 19(5): 100−113(in Chinese with English abstract).
Wang H C, Xiang Z Q, Zhao F Q, et al. 2012b. The alkaline plutons in eastern part of Guyang County, Inner Mongolia: Geochronology, petrogenesis and tectonic implications[J]. Acta Petrologica Sinica, 28(9): 2843−2854 (in Chinese with English abstract).
Wang H Z. 1979. Major stages of tectonic evolution of Asia[J]. Science in China, (12): 1187−1197(in Chinese).
Wang J, Lv H B, Zhang Y X, et al. 2012. Characteristics of ductile shear zone in the northern Bayan Obo ore deposits, North China and its structural significance[J]. Acta Geologica Sinica, 86(5): 785−792(in Chinese with English abstract).
Wang J, Li S Q, Wang B L, et al. 1992. The Langshan−Bayan Obo Rifting Valley[M]. Beijing: Peking University Publishing House: 1−136(in Chinese with English abstract).
Wang J P, Yang Y D. 1986. Discussion on genesis of thrusting tectonics in Daqingshan and adjacent region[C]//Contributions on Structural Geology(6). Beijing: Geological Publishing House: 1−16(in Chinese).
Wang K Y, Fan H R, Xie Y H, et al. 2001. Zircon U−Pb ages of basic complexes of the Bayan Obo REE−Nb−Fe deposit[J]. Chinese Science Bulletin, 46(16): 1390−1393(in Chinese). doi: 10.1360/csb2001-46-16-1390
Wang L, Wang G H, Lei S B, et al. 2015. Petrogenesis of Dahuabei pluton from Wulashan, Inner Mongolia: Constraints from geochemistry, zircon U−Pb dating and Sr−Nd−Hf isotopes[J]. Acta Petrologica Sinica, 31(7): 1977−1994(in Chinese with English abstract).
Wang M, Luo J L, L M, et al. 2013. Provenance and tectonic setting of sandstone−type uranium deposit in Dongsheng area, Ordos basin: Evidence from U−Pb age and Hf isotopes of detrital zircon[J]. Acta Petrologica Sinica, 29(8): 2746−2758(in Chinese with English abstract).
Wang P. 2015. The Xibiehe section and Xibiehe formation of the Bateaobao area in Darhan Mumingan Joint Banner, Inner Mongolia[J]. Journal of Jilin University(Earth Science Edition), 35(4): 409−414(in Chinese with English abstract).
Wang Q, Liu X Y, Li J Y. 1991. Plate Tectonics Between Cathaysia and Angaraland in China[M]. Beijing: Peking University Publishing House: 1−149 (in Chinese).
Wang Q, Liu X Y. 1986. Paleoplate tectonics between Cathaysia and Angaraland in Inner Mongolia of China[J]. Tectonics, 5: 1073−1088.
Wang T, Guo L, Zheng Y D, et al. 2012. Timing and processes of late Mesozoic mid−lower−crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton: Mainly constrained by zircon U–Pb ages from metamorphic core complexes[J]. Lithos, 154: 315−345. doi: 10.1016/j.lithos.2012.07.020
Wang W Q, Xu Z Y, Liu Z H, et al. 2013. Early−Middle Permian tectonic evolution of the central northern margin of the North China Craton: Constraints from zircon U−Pb ages and geochemistry of the granitoids[J]. Acta Petrologica Sinica, 29(9): 2987−3003(in Chinese with English abstract).
Wang X. 2018. Analysis on the ore−forming time and genesis of the Bayan Obo REE−Nb−Fe deposit: With a discussion on the mass extinction at the P−T boundary and “AMH” orogeny[J]. Geological Review, 64(2): 299−345(in Chinese with English abstract).
Wang X L, Zhang C, Liu S W, et al. 2007. Electron microprobe dating of monazite in granite from Kanbao area, Hebei Province[J]. Acta Petrologica Sinica, 23(4): 817−822(in Chinese with English abstract).
Wang X S, Zheng Y D, Zhang J J, et al. 2002. Extensional kinematics and shear type of the Hohhot metamorphic core complex, Inner Mongolia[J]. Geological Bulletin of China, 21(4/5): 238−245(in Chinese with English abstract).
Wang Z Q. 1925. Daqingshan coal Geology, Shuiyuan[J]. Geological Bulletin, 10: 1−42(in Chinese).
Wu F, Zhang S H, Zhao Y, et al. 2014. Emplacement depths of the Early Permian plutons in Guyang area of northern North China Block and their tectonic implications[J]. Geology in China, 41(3): 824−837(in Chinese with English abstract).
Wu F Y, Xu Y G, Zhu R X, et al. 2014. Thinning and destruction of the cratonic lithosphere: A global perspective[J]. Science China: Earth Sciences, 57(12): 2878−2890.
Wu T R, Zhang C, Wang J H. 1998. Tectonic settings of Ondor Sum group and its tectonic interpretation in Ondor Sun region, Inner Mongolia[J]. Geological Journal of China University, 4(2): 168−176(in Chinese with English abstract).
Xiao W, Windley B F, Hao J, et al. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: termination of the Central Asian Orogenic Belt[J]. Tectonics, 22(6): 1069.
Xie J B, Wang F H, Shang T. 2010. Deformation features of the ductile shear Zone and its age in Siziwangqi, Inner Mongolia[J]. Geological Suvey and Research, 33(4): 282−290(in Chinese with English abstract).
Xu B, Charvet J, Chen Y, et al. 2013. Middle Paleozoic convergent orogenic belts in western Inner Mongolia(China): Framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt[J]. Gondwana Research, 23(4): 1342−1364. doi: 10.1016/j.gr.2012.05.015
Xu B, Zhao P, Bao Q Z, et al. 2014. Preliminary study on the pre−Mesozoic tectonic unit division of the Xing−Meng orogenic belt(XMOB)[J]. Acta Petrologica Sinica, 30(7): 1841−1857(in Chinese with English abstract).
Xu B W, Xi A H, Ge Y H, et al. 2015. Zircon U−Pb ages of the Late Paleozoic A−type granites in chifeng, Inner Mongolia and its tectonic significance[J]. Acta Geologica Sinica, 2015,89(1): 58−69 (in Chinese with English abstract).
Xu D K. 1987. Stratigraphic and petrochemical characteristics of a fossil volcanic island−arc rock series: Baoerhantu group with a discussion of its genesis[C]//Contributions to the Project of Plate Tectonics in Morthern China. Beijing: Geological Publishing House: 101−112 (in Chinese with English abstract).
Xu L Q, Deng J F, Chen Z Y, et al. 2003. The identification of Ordovician adakites and its signification in northern Damao, Inner Mongolia[J]. Geoscience, 17(4): 428−434(in Chinese with English abstract).
Xu Z Y, LiuZ H, Yang Z S. 2001. Mesozoic orogenic movement and tectonic evolution in Daqingshan region, Inner Mongolia[J]. Journal of Changchun University of Science and Technology, 31(4): 317−322(in Chinese with English abstract).
Xu Z Q, Zhang G W. 2013. Progress in tectonics and dynamics of China (East Asia)––Forum on Frontiers of Science & Technology: Tectonics and Dynamics of China (East Asia)[J]. Scientia Sinica Terrae, 43: 1527−1538(in Chinese). doi: 10.1360/zd-2013-43-10-1527
Yan G H, Mu B L, Xu B L, et al. 2000. Chronologic ages and Sr−Nb−Pb isotopic features of Triassic alkaline intrusion in Yanshan−Yinshan area and their significance[J]. Science in China(Series D), 30(4): 383−387(in Chinese).
Yang X P, Ran Y K, Hu B, et al. 2002. Active Fault and Paleoearthquakes of the piedmont fault (Wujumengkou−Dongfeng Village) for Seertang Mountains, Inner Mongolia[J]. Earthquake Research in China, 18(2): 127−140 (in Chinese with English abstract).
Yang X P, Ran Y K, Hu B, et al. 2003. Paleoseismic activity on Wujiahe segment of Seerteng piedmont fault, Inner Mongolia[J]. Acta Seismologica Sinica, 25(1): 62−67. (in Chinese with English abstract).
Ye H, Zhang S H, Zhao Y, et al. 2014. Recognition of the latest Devonian volcanic rocks in Chifeng area, northern North China block, and its geological implications[J]. Geological Bulletin of China, 33(9): 1274−1283 (in Chinese with English abstract).
Yuan G B, Wang H C. 2006. Early Permian magmatic activities in northwest Wuchuan, Inner Mongolia and its tectonic significance[J]. Geological Survey and Research, 29(4): 303−310(in Chinese with English abstract).
Zeng J J, Zheng Y Y, Qi J H, et al. 2008. Foundation and geological significance of Adakitic granit at Guyang of Inner Mongolia[J]. Earth Science, 33(6): 755−763(in Chinese with English abstract).
Zeng Q D, Yang J H, Liu J M, et al. 2012. Genesis of the Chehugou Mo−bearing granitic complex on the northern margin of the North China Craton: geochemistry, zircon U−Pb age and Sr−Nd−Pb isotopes[J]. Geol. Mag., 149(5): 753−767. doi: 10.1017/S0016756811000987
Zhang C H. 1996. Research on the Intracontinental Structures and Orogeny in Yanshan area[D]. Doctoral Thesis of China University of Geology (Beijing) (in Chinese with English abstract).
Zhang C H. 1999. A primary discussion on the intraplate orogenic belt[J]. Earth Science Frontiers, 6(4): 295−308(in Chinese with English abstract).
Zhang G W, Guo A L, Wang Y J, et al. 2013. Tectonics of South China continent and its implications[J]. Science China: Earth Sciences, 56: 1804−1828(in Chinese). doi: 10.1007/s11430-013-4679-1
Zhang J F, Liu Z H, Guan Q B, et al. 2017. Age and geological significance of Xuniwusu formation from Bainaimiao area of Sonid Youqi, Inner Mongolia[J]. Acta Petrologica Sinica, 33(10): 3147−3160(in Chinese with English abstract).
Zhang J J, Qi G W, Guo L, et al. 2009. 40Ar−39Ar dating of the Mesozoic thrusting in Daqingshan thrust−nappe system, Inner Mongolia, China[J]. Acta Petrologica Sinica, 25(3): 609−620(in Chinese with English abstract).
Zhang Q Q, Zhang S H, Zhao Y, et al. 2018. Devonian alkaline magmatic belt along the northern margin of the North China Block: Petrogenesis and tectonic implications[J]. Lithos, 302/303: 496−518. doi: 10.1016/j.lithos.2018.01.019
Zhang Q Q, Zhang S H. 2019. Devonian magmatism in the northern margin of the North China block and its tectonic setting[J]. Journal of Geomechanics, 25(1): 125−138(in Chinese with English abstract).
Zhang S H, Zhao Y, Song B. 2006. Hornblende thermobarometry of the Carboniferous granitoids from the Inner Mongolia Paleo− uplift: Implications for the tectonic evolution of the northern margin of North China block[J]. Mineralogy and Petrology, 87: 123−141. doi: 10.1007/s00710-005-0116-2
Zhang S H, Zhao Y, Song B, et al. 2007. Petrogenesis of the middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications[J]. Geological Magazine, 144(3): 553−568. doi: 10.1017/S0016756807003275
Zhang S H, Zhao Y, Liu J, et al. 2007. Emplacement depths of the Late Paleozoic−Mesozoic granitiod intrusions from the northern North China block and their tectonic implications[J]. Acta Petrologica Sinica, 23(3): 625−638(in Chinese with English abstract).
Zhang S H, Zhao Y, Song B, et al. 2009a. Contrasting Late Carboniferous and Late Permian–Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications[J]. GSA Bulletin, 121(1/2): 181−200.
Zhang S H, Zhao Y, Liu X C, et al. 2009b. Late Paleozoic to Early Mesozoic mafic−ultramafic complexes from the northern North China Block: constraints on the composition and evolution of the lithospheric mantle[J]. Lithos, 110: 229–246.
Zhang S H, Zhao Y, Ye H, et al. 2014. Origin and evolution of the Bainaimiao arc belt: Implications for crustal growth in the southern Central Asian Orogenic Belt[J]. Geological Society of America Bulletin, 126(9/10): 1275−1300.
Zhang W, Jian P. 2008. SHRIMP dating of early Paleozoic granites from north Damaoqi, Inner Mongolia[J]. Acta Geologica Sinica, 82(6): 778−787(in Chinese with English abstract).
Zhang W Jian P, Liu D Y, et al. 2012. SHRIMP dating of the Permian Guyang diorite−quartz diorite−tonalite suite in the northern margin of the North China craton[J]. Geology in China, 39(6): 1593−1603(in Chinese with English abstract).
Zhang W, Jian P, Kröner A, et al. 2013. Magmatic and metamorphic development of an early to mid−Paleozoic continental margin arc in the southernmost Central Asian Orogenic Belt, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 72: 63−74. doi: 10.1016/j.jseaes.2012.05.025
Zhang X H, Zhang H F, Jiang N, et al. 2010. Early Devonian alkaline intrusive complex from the northern North China Craton: A petrological monitor of post−collisional tectonics[J]. Journal of the Geological Society, 167(4): 717−730. doi: 10.1144/0016-76492009-110
Zhang Y P, Tang K D. 1989. Pre−Jurassic tectonic ebolution of intercontinental region and the suture zone between the Norht China and Siberian platform[J]. Journal of Southeast Asian Earth Sciences, 3(1/4): 47−55.
Zhang Y P, Su Y Z, Li J C. 2010. Regional tectonics significance of the Late Silurian Xibiehe Formation in central Inner Mongolia, China[J]. Geological Bulletin of China, 29(11): 1599−1605(in Chinese with English abstract).
Zhang Y Q, Teng J W, Wang Q S, et al. 2013. Crustal structure and the geodynamic process beneath the Hetao basin and adjacent area[J]. Progress in Geophysics, 28(5): 2264−2272(in Chinese with English abstract).
Zhang Y Q, Su H W. 2002. U−Pb ssingle zircon ages of metamorphic basic volcanic rocks of Baoyintu rock group in Inner Mongolia[J]. Progress in Precambrian Research, 25(3/4): 199−204(in Chinese with English abstract).
Zhang Y Q. 2004. Ages, tectonic environment and geological significance of metabasic volcanic rocks of the Buyant group−complex in the north of Bayan Obo, Inner Mongolia[J]. Geological Bulletin of China, 23(2): 177−183(in Chinese with English abstract).
Zhang Y X, Jiang S Q, Zhang Q L, et al. 2008. A discussion on forming time of the Bayan Obo Group and ore−forming time of the Bayan Obo giant REE−Nb−Fe deposit, Inner Mongolia[J]. Geology in China, 35(6): 1129−1137(in Chinese with English abstract).
Zhang Y X, Liu J Y. 2010. Discovery of big fossil in Sailinghudong group in Heinaobao of Damaoqi, Inner Mongolia[J]. Geological Review, 56(1): 123−124(in Chinese).
Zhao L, Wu T R, Luo H L. 2011. SHRIMP U−Pb dating, geochemistry and tectonic implications of the Beiqigetao gabbros in Uradzhongqi area, Inner Mongolia[J]. Acta Petrologica Sinica, 27(10): 3072−3082(in Chinese with English abstract).
Zhao L G, Li C D, Chang Q S, et al. 2016. A tentative discussion on zircon U−Pb geochronology and geochemistry of ore−bearing intermediate−acid intrusive rocks in the Bainaimiao copper ore district and the metallogenic epoch[J]. Geological Bulletin of China, 35(4): 542−552(in Chinese with English abstract).
Zhao L G, Wang W L, Gao X S, et al. 2024. Inspiration from the age of Baoerhantu group and metamorphic zircon age of Middle Early−Middle Triassic in the northern Damao Banner, Inner Mongolia[J]. North China Geology, 47(2): 1−16 (in Chinese with English abstract).
Zheng Y D, Davis G A, Wang C, et al. 1998. Major thrust sheet in the Daqing Shan Mountains, Inner Mongolia, China[J]. Science in China(Series D), 41(5): 553−560.
Zheng Y F, Wu F Y. 2009. Growth and reworking of cratonic lithosphere[J]. Chinese Sci. Bull., 54: 1945−1949(in Chinese). doi: 10.1360/csb2009-54-14-1945
Zhou J B, Zheng Y F, Yang X Y, et al. 2002. Paleoplate tectonics and regional geology at Bayan Obo in northern Inner Mongolia[J]. Geological Journal of China University, 8(1): 46−61(in Chinese with English abstract).
Zhou Z G, Zhang H F, Liu H L, et al. 2009. Zircon U−Pb dating of basic intrusions in Siziwangqi area of middle Inner Mongolia, China[J]. Acta Petrologica Sinica, 25(6): 1519−1528(in Chinese with English abstract).
Zhou Z G, Wang G S, Zhang D, et al. 2016. Zircon ages of gabbros in the Siziwangqi, Inner Mongolia and its constrain on the formation time of the Bayan Obo Group[J]. Acta Petrologica Sinica, 32(6): 1809−1822(in Chinese with English abstract).
Zhou Z G, Zhang D, Gu Y C, et al. 2018. Characteristics of Bainaimiao thrust belt along central Inner Mongolia in North China and its geological significance[J]. Geotectonica et Metallogenia, 42(1): 1−17(in Chinese with English abstract).
Zhou Z H, Mao J W, Ma X H, et al. 2017. Geochronological framework of the Early Paleozoic Bainaimiao Cu−Mo−Au deposit, NE China, and its tectonic implications[J]. Journal of Asian Earth Sciences, 144: 323−338. doi: 10.1016/j.jseaes.2016.11.005
Zhu R X, Chen L, Wu F Y, et al. 2011. Timing, scale and mechanism of the destruction of the North China Craton[J]. Scienc China Earth Sciences, 54(6): 789−797(in Chinese). doi: 10.1007/s11430-011-4203-4
Zhu R X, Xu Y G, Zhu G, et al. 2012. Destruction of the North China craton[J]. Sci. China Earth Sci., 42(8): 1135−1159(in Chinese).
Zhu S Y. 1997. Nappe tectonics in Sertengshan−Daqingshan, Inner Mongolia[J]. Geology of Inner Mongolia, 84(1): 41−47(in Chinese with English abstract).
Zhu W P, Tian W, Wei C J. 2023. Discovery of the Late Carboniferous alkaline volcanic rocks in the Guyang area, eastern Yinshan Block, and its geological implications[J]. Acta Petrologica Sinica, 39(3): 670−688(in Chinese with English abstract).
白新会, 徐仲元, 刘正宏, 等. 2015. 中亚造山带东段南缘早志留世岩体锆石U−Pb定年、地球化学特征及其地质意义[J]. 岩石学报, 31(1): 67−69. 陈崎, 仇甘霖, 杜玉申, 等. 1992. 白乃庙—温都尔庙区域构造及华北北缘古板块构造演化[J]. 长春地质学院学报, (22): 119−129. 陈志勇, 温长顺, 张维杰. 2000. 内蒙古色尔腾山的推覆构造[J]. 地球科学, 25(3): 237−282. doi: 10.3321/j.issn:1000-2383.2000.03.004 陈志勇, 李玉玺, 王新亮. 2002. 包头—呼和浩特北部地区逆冲推覆构造[J]. 地质通报, 21(4/5): 251−258. 程绍平, 邓起东, 杨桂枝, 等. 2000. 内蒙古大青山的新生代剥蚀和隆起[J]. 地震地质, 22(1): 27−36. doi: 10.3969/j.issn.0253-4967.2000.01.004 初航, 张晋瑞, 魏春景, 等. 2013. 内蒙古温都尔庙群变质基性火山岩构造环境及年代新解[J]. 科学通报, 58(28/29): 2958−2965. 党智财, 李俊建, 赵泽霖, 等. 2016. 内蒙古四子王旗地区小南山辉长岩LA−ICP−MS锆石U−Pb年龄及其地质意义[J]. 地质通报, 35(4): 583−592. doi: 10.3969/j.issn.1671-2552.2016.04.014 党智财, 李俊建, 付超, 等. 2018. 内蒙古乌拉特中旗克布镁铁质-超镁铁质岩体年代学、矿物学和岩石地球化学[J]. 地质学报, 92(2): 278−297. doi: 10.3969/j.issn.0001-5717.2018.02.006 董春艳, 马铭株, 颉颃强, 等. 2021. 白云鄂博地区早前寒武纪基底岩浆作用和变质作用: 锆石SHRIMP U−Pb定年和LA−MC−ICPMS Hf同位素分析[J]. 岩石学报, 37(2): 417−432. doi: 10.18654/1000-0569/2021.02.06 杜菊民, 张庆龙, 徐士银, 等. 2009. 阴山晚中生代板内造山特征及其动力机制——以内蒙古大青山为例[J]. 地质学报, 83(7): 910−922. doi: 10.3321/j.issn:0001-5717.2009.07.002 范宏瑞, 胡芳芳, 陈福坤, 等. 2006. 白云鄂博超大型REE−Nb−Fe矿区碳酸岩墙的侵位年龄——兼答Le Bas博士的质疑[J]. 岩石学报, 22(2): 519−520. doi: 10.3321/j.issn:1000-0569.2006.02.027 范宏瑞, 胡芳芳, 杨奎锋, 等. 2009. 内蒙古白云鄂博地区晚古生代闪长质-花岗质岩石年代学框架及其地质意义[J]. 岩石学报, 25(11): 2933−2938. 范宏瑞, 杨奎锋, 胡芳芳, 等. 2010. 内蒙古白云鄂博地区基底岩石锆石年代学及对构造背景的指示[J]. 岩石学报, 26(5): 1342−1350. 酆少英, 刘保金, 姬计法, 等. 2015. 呼和浩特−包头盆地岩石圈细结构的深地震反射探测[J]. 地球物理学报, 58(4): 1158−1168. doi: 10.6038/cjg20150406 冯帆, 徐仲元, 董晓杰, 等. 2021. 内蒙古温都尔庙—集宁地区花岗斑岩年代学、地球化学、Hf同位素特征及其地质意义[J]. 地球科学, 46(6): 1973−1992. 冯丽霞, 张志诚, 韩宝福, 等. 2013. 内蒙古达茂旗花岗岩类LA−ICP−MS锆石U−Pb年龄及其地质意义[J]. 地质通报, 32(11): 1737−1748. doi: 10.3969/j.issn.1671-2552.2013.11.006 高德臻, 李龙, 张维杰. 2001. 内蒙古临河-集宁断裂带中段构造特征及其演化[J]. 中国区域地质, 20(4): 337−342. 葛肖虹. 1989. 华北板内造山带的形成史[J]. 地质论评, 35(3): 254−261. doi: 10.3321/j.issn:0371-5736.1989.03.009 龚弥, 蔡剑辉, 阎国翰, 等. 2019. 阴山-燕山北麓富碱侵入岩体的岩石地球化学特征、锆石 SHRIMP U−Pb 年龄及构造意义[J]. 地质论评, 65(4): 894−913. 郝百武, 蒋杰. 2010. 内蒙古镶黄旗哈达庙金矿杂岩体年代学、地球化学及其形成机制[J]. 岩石矿物学杂志, 29(6): 750−762. doi: 10.3969/j.issn.1000-6524.2010.06.012 和政军, 李锦轶, 牛宝贵, 等. 1998. 燕山—阴山地区晚侏罗世强烈推覆-隆升事件即沉积响应[J]. 地质论评, 44(4): 407−418. doi: 10.3321/j.issn:0371-5736.1998.04.010 和政军, 王宗起, 任纪舜. 1999. 华北北部侏罗纪大型推覆构造带前缘盆地沉积特征和成因机制初探[J]. 地质科学, 34(2): 186−195. 侯建光, 苏尚国, 周岱, 等. 2014. 内蒙温根南基性—超基性岩体岩石学、地球化学特征及其形成构造背景[J]. 岩石学报, 30(12): 3729−3740. 胡晓. 1983. 内蒙地槽区的蓝闪片岩及其地质特征[C]//中国北方板块构造论文集. 沈阳: 沈阳地质矿产研究所: 230−242. 胡晓. 1985. 内蒙古温都尔庙早古生代板块俯冲带的俯冲速度和消减深度[J]. 河北地质学院学报, (4): 33−40. 胡晓, 许传诗, 牛树银. 1990. 华北地台北缘早古生代大陆边缘演化[M]. 北京: 北京大学出版社: 1−215. 胡晓, 牛树银. 1992. 内蒙古狼山一渣尔泰山中元古界的构造变形与演化[J]. 中国区域地质, (1): 75−82. 胡晓佳, 杨泽黎, 王树庆, 等. 2022. 内蒙古包尔汉图岛弧早古生代火山岩年代学、地球化学特征、岩石成因及对兴蒙造山带构造演化的约束[J]. 地质学报, 96(3): 897−817. doi: 10.3969/j.issn.0001-5717.2022.03.011 黄汲清. 1960. 中国地质构造基本特征的初步总结[J]. 地质学报, 40(1): 1−32. 黄汲清, 任纪舜, 姜春发, 等. 1977. 中国大地构造基本轮廓[J]. 地质学报, (2): 117−135. 黄汲清. 1979. 对中国大地构造特点的一些认识并着重讨论地槽褶皱带的多旋回发展问题[J]. 地质学报, (2): 99−111. 黄汲清. 1984. 中国大地构造特征的新研究[J]. 中国地质科学院院报, 9: 5−18. 贾炳文, 武永强. 1995. 内蒙古大青山晚古生代煤系中火山事件层的物质来源及地层意义[J]. 华北地质矿产杂志, 10(2): 203−213. 贾和义, 宝音乌力吉, 张玉清. 2003. 内蒙古达茂旗乌德缝合带特征及大地构造意义[J]. 成都理工大学学报(自然科学版), 30(1): 30−34. 简平, 刘敦一, 张旗, 等. 2003. 蛇绿岩及蛇绿岩中浅色岩的SHRIMP U−Pb测年[J]. 地学前缘, 10(4): 439−456. doi: 10.3321/j.issn:1005-2321.2003.04.012 靳胜凯, 刘博, 马明, 等. 2024. 内蒙古化德地区二叠纪—三叠纪侵入岩年代学及地球化学特征: 对古亚洲洋东段构造演化的制约[J]. 地质学报, 98(1): 116−137. 康玉柱. 2007. 中国主要构造体系及控油作用研究[J]. 中国西部油气地质, 3(1): 1−8. 冷柚兵, 张元厚, 陈跃军, 等. 2019. 内蒙古中部朱日和地区变质玄武岩特征及其意义[J]. 世界地质, 3(3): 598−610. doi: 10.3969/j.issn.1004-5589.2019.03.003 李承东, 冉皞, 赵利刚, 等. 2012. 温都尔庙群锆石的LA−MC−ICPMS U−Pb年龄及其构造意义[J]. 岩石学报, 28(11): 3705−3714. 李春昱, 王荃, 刘雪亚, 等. 1982. 亚洲大地构造图(比例尺1∶800万)及说明书[M]. 北京: 地图出版社. 李春昱, 汤耀庆. 1983. 亚洲古板块划分以及有关问题[J]. 地质学报, (1): 1−10. 李刚, 刘正宏, 徐仲元, 等. 2012. 内蒙古白乃庙逆冲推覆构造的组成及其构造特征[J]. 吉林大学学报(地球科学版), 42(1): 301−319. 李继亮, 胡辅佑. 1981. 白云鄂博群中蛇纹岩质滑塌堆积[J]. 地质科学, 16(3): 269−273. 李建锋, 张志诚, 韩宝福. 2010. 内蒙古达茂旗北部闪长岩锆石 SHRIMP U−Pb、角闪石40Ar/39Ar 年代学及其地质意义[J]. 岩石矿物学杂志, 29(6): 732−740. doi: 10.3969/j.issn.1000-6524.2010.06.010 李锦轶, 何国琦, 徐新, 等. 2006. 新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J]. 地质学报, 80(1): 148−168. doi: 10.3321/j.issn:0001-5717.2006.01.017 李锦轶, 高立明, 孙桂华, 等. 2007. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J]. 岩石学报, 23(3): 565−582. doi: 10.3969/j.issn.1000-0569.2007.03.004 李锦轶. 2009. 中国大陆地质历史上的旋回与阶段[J]. 中国地质, 36(3): 504−521. doi: 10.3969/j.issn.1000-3657.2009.03.003 李锦轶, 张进, 杨天南, 等. 2009. 北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J]. 吉林大学学报(地球科学版), 39(4): 584−605. 李锦轶, 张进, 刘建峰, 等. 2014. 中国大陆主要变形系统[J]. 地学前缘, 21(3): 226−245. 李锦轶, 刘建峰, 曲军峰, 等. 2019a. 中国东北地区主要地质特征和地壳构造格架[J]. 岩石学报, 35(10): 2989−3016. 李锦轶, 张进, 刘建峰, 等. 2019b. 中国地壳结构构造与形成过程: 来自构造变形的约束[J]. 地质力学学报, 25(5): 678−698. 李俊建, 党智财, 赵泽霖, 等. 2015. 内蒙古白乃庙铜矿床成矿时代的研究[J]. 地质学报, 89(8): 1448−1457. doi: 10.3969/j.issn.0001-5717.2015.08.008 李尚启, 陈跃军, 韩仁道, 等. 2017. 内蒙古温都尔庙地区白音诺尔一带变质基性火山岩年代学和地球化学研究[J]. 世界地质, 36(2): 428−440. doi: 10.3969/j.issn.1004-5589.2017.02.010 李文博, 陈衍景, 赖勇, 等. 2018. 内蒙古白乃庙铜金矿床的成矿时代和成矿构造背景[J]. 岩石学报, 24(4): 890−898. 李仰春, 李智佩, 古永昌, 等. 2020. 中华人民共和国地质图(比例尺1∶150万) [M]. 北京: 地质出版社. 李玉玺, 胡凤翔, 陈志勇, 等. 2002. 内蒙古旗下营北部神水梁一带伸展构造[J]. 地质通报, 21(4/5): 259−263. 刘敦一, 简平, 张旗, 等. 2003. 内蒙古图林凯蛇绿岩中的埃达克岩SHRIMP测年: 早古生代洋壳消减的证据[J]. 地质学报, 77(3): 317−327. doi: 10.3321/j.issn:0001-5717.2003.03.004 刘建峰, 李锦轶, 迟效国, 等. 2013. 华北克拉通北缘与弧-陆碰撞相关的早泥盆世长英质火山岩——锆石 U-Pb 定年及地球化学证据[J]. 地质通报, 32(2/3): 267−278. 刘江, 张进江, 郭磊, 等. 2014. 内蒙古呼和浩特变质核杂岩韧性拆离带40Ar−39Ar定年及其构造含义[J]. 岩石学报, 30(7): 1899−1908. 刘兰笙, 高翎, 杜安道, 等. 1996. 白云鄂博稀土矿床中辉钼矿的铼-锇同位素年龄[J]. 矿床地质, 15(2): 188−191. 刘玉龙, 杨刚, 陈江峰, 等. 2005. 白云鄂博超大型稀土-铌-铁矿床黄铁矿Re−Os定年[J]. 科学通报, 50(2): 172−175. doi: 10.3321/j.issn:0023-074X.2005.02.012 刘正宏, 徐仲元, 杨振升. 1999. 论内蒙古大青山地区逆冲推覆构造[J]. 中国区域地质, 18(4): 366−372. 刘正宏, 徐仲元, 杨振升. 2001. 大青山逆冲推覆体系含义及地质特征[J]. 世界地质, 20(3): 223−230. doi: 10.3969/j.issn.1004-5589.2001.03.003 刘正宏, 徐仲元, 杨振升. 2002. 阴山中生代地壳逆冲推覆与伸展变形作用[J]. 地质通报, 21(4/5): 246−230. doi: 10.3969/j.issn.1671-2552.2002.04.011 刘正宏, 徐仲元, 杨振升. 2003a. 大青山逆冲推覆构造形成时代的40Ar/39Ar年龄证据[J]. 科学通报, 48(20): 2193−2197. doi: 10.3321/j.issn:0023-074X.2003.20.018 刘正宏, 徐仲元. 杨振升. 2003b. 内蒙古大青山印支运动厘定[J]. 地质论评, 49(5): 457−463. doi: 10.3321/j.issn:0371-5736.2003.05.002 柳长峰, 杨帅师, 武将伟, 等. 2010. 内蒙古中部四子王旗地区晚二叠—早三叠世过铝花岗岩定年及成因[J]. 地质学报, 84(5): 1012−1016. 柳长峰, 刘文灿, 周志广. 2014a. 内蒙古四子王旗地区古生代—早中生代侵入岩活动期次、特征及构造背景[J]. 地质学报, 88(6): 992−1002. 柳长峰, 刘文灿, 王惠平, 等. 2014b. 华北克拉通北缘白乃庙组变质火山岩锆石定年与岩石地球化学特征[J]. 地质学报, 88(7): 1273−1287. 卢俊生, 倪志耀, 翟明国, 等. 2009. 冀北赤城红旗营子群中变质橄榄岩的岩石学与地球化学特征[J]. 矿物岩石, 29(3): 91−99. doi: 10.3969/j.issn.1001-6872.2009.03.014 鲁颖淮, 李文博, 赖勇. 2009. 内蒙古镶黄旗哈达庙金矿床含矿斑岩体形成时代和成矿构造背景[J]. 岩石学报, 25(10): 2615−2620. 罗红玲, 吴泰然, 李毅. 2007. 乌拉特中旗克布岩体的地球化学特征及SHRIMP定年: 早二叠世华北克拉通底侵作用的证据[J]. 岩石学报, 23(4): 756−763. 罗红玲, 吴泰然, 赵磊. 2009. 华北板块北缘乌梁斯太A型花岗岩体锆石 SHRIMP U−Pb 定年及构造意义[J]. 岩石学报, 25(3): 515−526. 罗镇宽, 苗来成, 关康, 等. 2001. 河北张家口水泉沟岩体SHRIMP 年代学研究及其意义[J]. 地球化学, 30(2): 116−122. doi: 10.3321/j.issn:0379-1726.2001.02.002 吕钊, 王建平, 王继春, 等. 2022. 内蒙古白乃庙铜金矿床侵入岩年代学及其地质意义[J]. 现代地质, 36(1): 307−319. 马阁, 申萍, 潘鸿迪, 等. 2019. 内蒙古白乃庙铜金矿床含矿斑岩地球化学、锆石U−Pb年代学、微量元素地球化学及成矿指示意义[J]. 地质学报, 93(12): 3144−3165. doi: 10.3969/j.issn.0001-5717.2019.12.010 马云飞, 焦建刚, 郭天牧, 等. 2022. 内蒙古四子王旗小南山地区镁铁质—超镁铁质岩体岩石成因及含矿性评价[J]. 地质学报, 96(12): 4312−4330. doi: 10.3969/j.issn.0001-5717.2022.12.016 苗来成, Qiu M, 关康, 等. 2001a. 内蒙古乌拉山地区大桦背岩体SHRIMP U−Pb年代学研究[J]. 地质论评, 47(2): 169−173. 苗来成, 翟裕生, 朱成伟, 等. 2001b. 冀西北水泉沟碱性杂岩体成岩时代研究[J]. 黄金地质, 7(1): 1−6. 内蒙古自治区地质矿产局. 1991. 内蒙古自治区区域地质志[M]. 北京: 地质出版社: 1−725. 聂凤军, 裴荣富, 吴良士. 1995. 内蒙古白乃庙地区绿片岩和花岗闪长斑岩的钕和锶同位素研究[J]. 地球学报, (1): 36−44. 彭立红. 1984. 内蒙温都尔庙群南带蛇录岩套的地质时代及其大地构造意义[J]. 科学通报, 29(2): 104−107. 乔秀夫, 高林志, 彭阳, 等. 1997. 内蒙古腮林忽洞群综合地层和白云鄂博矿床赋矿微晶丘[J]. 地质学报, 71(3): 202−211. doi: 10.3321/j.issn:0001-5717.1997.03.001 戚国伟, 张进江, 王新社, 等. 2007. 内蒙古大青山中生代逆冲-伸展构造格局及空间关系[J]. 自然科学进展, 17(3): 329−338. doi: 10.3321/j.issn:1002-008X.2007.03.007 祁思敬, 胡骁, 丁溥权, 等. 1979. 内蒙古板块运动的证据及与地槽演化的关系[J]. 河北地质学院学报, (3): 1−13. 秦亚, 梁一鸣, 邢济麟, 等. 2013. 内蒙古正镶白地区早古生代O型埃达克岩的厘定及其意义[J]. 地学前缘, 20(5): 106−114. 任纪舜, 王作勋, 陈炳蔚, 等. 1999. 从全球看中国大地构造——中国及邻区大地构造图简要说明[M]. 北京: 地质出版社: 1−50. 任英忱, 张英臣, 张宗清. 1994. 白云鄂博稀土超大型矿床的成矿时代及其主要地质热事件[J]. 地球学报, (Z1): 95−101. 尚恒胜, 陶继雄, 宝音乌力吉, 等. 2003. 内蒙古白云鄂博地区早古生代弧−盆体系及其构造意义[J]. 地质调查与研究, 26(3): 160−168. 邵济安. 1991. 中朝板块北缘中段的地壳演化[M]. 北京: 北京大学出版社: 1−136. 苏文博, 李文国, 李惠民, 等. 2022. 什那干群层凝灰岩夹层SHRIMP锆石U−Pb年代学研究及其意义[J]. 华北地质, 45(2): 51−67. 苏养正, 唐克东, 池永一, 等. 1983. 内蒙古白云鄂博东北上志留统西别河组新资料[C]//中国北方板块构造文集编委会. 中国北方板块构造论文集. 沈阳: 沈阳地质矿产研究所: 221−229. 孙立新, 任邦方, 滕飞, 等. 2015. 内蒙古敖汉旗朝吐沟组火山岩LA−ICP−MS锆石U−Pb年龄[J]. 地质通报, 34(8): 1493−1501. doi: 10.3969/j.issn.1671-2552.2015.08.009 孙立新, 张云, 李影, 等. 2017. 内蒙古赤峰地区晚泥盆世双峰式火山岩地球化学特征与板内伸展事件[J]. 中国地质, 44(2): 371−388. 唐克东. 1983. 论温都尔庙群及其构造意义[C]//唐克东主编. 中国北方板块构造文集. 沈阳: 沈阳地质矿产研究所: 186−208. 唐克东. 1992. 中朝板块北侧褶皱带构造演化及成矿规律[M]. 北京: 北京大学出版社: 1−277. 唐克东, 颜竹筠, 张允平, 等. 1983. 关于温都尔庙群及其构造意义[C]//唐克东主编. 中国北方板块构造文集. 沈阳: 沈阳地质矿产研究所: 186−205. 田涛, 倪志耀, 潘登, 等. 2018. 冀北康保晚古生代花岗质岩浆作用年龄数据及构造意义[J]. 地质科学, 53(2): 661−667. doi: 10.12017/dzkx.2018.036 王荃, 刘雪亚, 李锦轶. 1991. 中国华夏与安加拉古陆间的板块构造[M]. 北京: 北京大学出版社. 汪彪, 施立志, 阮壮, 等. 2022. 内蒙古正镶白旗贡淖尔地区中二叠统额里图组下段细碎屑岩地球化学特征及意义[J]. 地球学报, 43(4): 569−583. doi: 10.3975/cagsb.2021.113001 汪相. 2018. 白云鄂博超大型稀土-铌-铁矿床的成矿时代及成因探析——兼论P-T之交生物群灭绝事件和“阿蒙兴造山运动”[J]. 地质论评, 64(2): 299−345. 王鸿祯. 1979. 亚洲地质构造发展的主要阶段[J]. 中国科学, (12): 1187−1197. 王惠初, 袁桂邦, 辛后田, 等. 1999. 内蒙古固阳下湿壕−武川酒馆韧性剪切带的大地构造意义探讨[J]. 前寒武纪研究进展, 22(1): 12−20. 王惠初, 初航, 相振群, 等. 2012a. 华北克拉通北缘崇礼—赤城地区的红旗营子(岩)群: 一套晚古生代的变质杂岩[J]. 地学前缘, 19(5): 100−113. 王惠初, 相振群, 赵凤清, 等. 2012b. 内蒙古固阳东部碱性侵入岩: 年代学、成因与地质意义[J]. 岩石学报, 28(9): 2843−2854. 王楫, 李双庆, 王保良, 等. 1992. 狼山-白云鄂博裂谷系[M]. 北京: 北京大学出版社: 1-136. 王建平, 杨玉东. 1986. 大青山及邻区冲断推覆构造形成机制的讨论[C]//构造地质论丛(6). 北京: 地质出版社: 1−16. 王俊, 吕洪波, 章雨旭, 等. 2012. 白云鄂博矿区北部韧性剪切带特征及其构造意义[J]. 地质学报, 86(5): 785−792. doi: 10.3969/j.issn.0001-5717.2012.05.011 王凯怡, 范宏瑞, 谢奕汉, 等. 2001. 白云鄂博超大型REE−Fe−Nb矿床基底杂岩的锆石U−Pb年龄[J]. 科学通报, 46(16): 1390−1393. 王梁, 王根厚, 雷时斌, 等. 2015. 内蒙古乌拉山大桦背岩体成因: 地球化学、锆石U−Pb年代学及Sr−Nd−Hf同位素制约[J]. 岩石学报, 31(7): 1977−1994. 王盟, 罗静兰, 李杪, 等. 2013. 鄂尔多斯盆地东胜地区砂岩型铀矿源区及其构造背景分析[J]. 岩石学报, 29(8): 2746−2758. 王平. 2005. 内蒙古达茂旗巴特敖包地区的西别河剖面与西别河组[J]. 吉林大学学报(地球科学版), 35(4): 409−414. 王挽琼, 徐仲元, 刘正宏, 等. 2013. 华北板块北缘中段早中二叠世的构造属性: 来自花岗岩类锆石 U−Pb 年代学及地球化学的制约[J]. 岩石学报, 29(9): 2987−3003. 王新社, 郑亚东, 张进江, 等. 2002. 呼和浩特变质核杂岩伸展运动学特征及剪切作用类型[J]. 地质通报, 21(4/5): 238−245. doi: 10.3969/j.issn.1671-2552.2002.04.010 王鑫琳, 张臣, 刘树文, 等. 2007. 河北康保地区花岗岩独居石电子探针定年[J]. 岩石学报, 23(4): 817−822. doi: 10.3321/j.issn:1000-0569.2007.04.012 王竹泉. 1925. 绥远大青山煤田地质[J]. 地质汇报, 10: 1−42. 吴飞, 张拴宏, 赵越, 等. 2014. 华北地块北缘内蒙古固阳地区早二叠世岩体的侵位深度及其构造意义[J]. 中国地质, 41(3): 824−837. doi: 10.3969/j.issn.1000-3657.2014.03.011 吴福元, 徐义刚, 朱日祥, 等. 2014. 克拉通岩石圈减薄与破坏[J]. 中国科学: 地球科学, 44: 2358−2372. 吴泰然, 张臣, 万基虎. 1998. 内蒙古温都尔庙地区温都尔庙群的形成环境和构造意义[J]. 高校地质学报, 4(2): 168−176. 谢静博, 王风华, 尚婷, 等. 2011. 内蒙古盘羊山逆冲推覆构造系统的组合特征[J]. 地质调查与研究, 34(1): 23−28. 谢静博, 王风华, 尚婷. 2010. 内蒙古四子王旗韧性剪切带基本特征及其时代[J]. 地质调查与研究, 33(4): 282−290. 徐备, 赵盼, 鲍庆中, 等. 2014. 兴蒙造山带前中生代构造单元划分初探[J]. 岩石学报, 30(7): 1841−1857. 徐博文, 郗爱华, 葛玉辉, 等. 2015. 内蒙古赤峰地区晚古生代 A型花岗岩锆石U−Pb年龄及构造意义[J]. 地质学报, 2015,89(1): 58−69. 徐冬葵. 1987. 古火山岛弧岩系——包尔汗图群地层、岩石化学特征及其成因探讨[C]//中国北方板块构造论文集. 北京: 地质出版社: 101−112. 徐仲元, 刘正宏, 杨振升. 2001. 内蒙古大青山地区中生代造山运动及构造演化[J]. 长春科技大学学报, 31(4): 317−322. doi: 10.3969/j.issn.1671-5888.2001.04.002 许立权, 邓晋福, 陈志勇, 等. 2003. 内蒙古达茂旗北部奥陶纪埃达克岩类的识别及其意义[J]. 现代地质, 17(4): 428−434. doi: 10.3969/j.issn.1000-8527.2003.04.011 许志琴, 张国伟. 2013. 中国(东亚)大陆构造与动力学——科学与技术前沿论坛“中国(东亚)大陆构造与动力学”专题进展[J]. 中国科学: 地球科学, 43: 1527−1538. 阎国翰, 牟保磊, 许保良, 等. 2000. 燕辽-阴山三叠纪碱性侵入岩年代学和 Sr, Nd, Pb 同位素特征及意义[J]. 中国科学(D辑), 30(4): 383−387. doi: 10.3969/j.issn.1674-7240.2000.04.006 杨晓平, 冉勇康, 胡博, 等. 2002. 内蒙古色尔腾山山前断裂(乌句蒙口-东风村段)的断层活动与古地震事件[J]. 中国地震, 18(2): 127−140. doi: 10.3969/j.issn.1001-4683.2002.02.002 杨晓平, 冉勇康, 胡博, 等. 2003. 内蒙古色尔腾山山前断裂带乌加河段古地震活动[J]. 地震学报, 25(1): 62−67. doi: 10.3321/j.issn:0253-3782.2003.01.008 叶浩, 张拴宏, 赵越, 等. 2014. 内蒙古赤峰地区泥盆纪晚期火山岩的发现及其地质意义[J]. 地质通报, 33(9): 1274−1283. doi: 10.3969/j.issn.1671-2552.2014.09.002 袁桂邦, 王惠初. 2006. 内蒙古武川西北部早二叠世岩浆活动及其构造意义[J]. 地质调查与研究, 29(4): 303−310. 曾俊杰, 郑有业, 齐建宏, 等. 2008. 内蒙古固阳地区埃达克质花岗岩的发型及其地质意义[J]. 地球科学, 33(6): 755−763. doi: 10.3321/j.issn:1000-2383.2008.06.003 张长厚. 1996. 燕山中生代陆内造山作用构造研究[D]. 中国地质大学(北京)博士学位论文. 张长厚. 1999. 初论板内造山带[J]. 地学前缘, 6(4): 295−308. doi: 10.3321/j.issn:1005-2321.1999.04.012 张国伟, 郭安林, 王岳军, 等. 2013. 中国华南大陆构造与问题. 中国科学: 地球科学, 43: 1553−1582. 张进江, 戚国伟. 郭磊, 等. 2009. 内蒙古大青山逆冲推覆体系中生代逆冲构造活动的40Ar−39Ar定年[J]. 岩石学报, 25(3): 609−620. 张金凤, 刘正宏, 关庆彬, 等. 2017. 内蒙古苏尼特右旗白乃庙地区徐尼乌苏组的形成时代及其地质意义[J]. 岩石学报, 33(10): 3147−3160. 张琪琪, 张拴宏. 2019. 华北地块北缘泥盆纪岩浆活动及其构造背景[J]. 地质力学学报, 25(1): 125−138. doi: 10.12090/j.issn.1006-6616.2019.25.01.012 张拴宏, 赵越, 刘健, 等. 2007. 华北地块北缘晚古生代—中生代花岗岩体侵位深度及其构造意义[J]. 岩石学报, 23(3): 625−638. doi: 10.3969/j.issn.1000-0569.2007.03.010 张维, 简平. 2012. 华北北缘固阳二叠纪闪长岩-石英闪长岩-英云闪长岩岩套SHRIMP年代学[J]. 中国地质, 39(6): 1593−1603. doi: 10.3969/j.issn.1000-3657.2012.06.009 张维, 简平. 2008. 内蒙古达茂旗北部早古生代花岗岩类SHRIMP U−Pb年代学[J]. 地质学报, 82(6): 778−787. doi: 10.3321/j.issn:0001-5717.2008.06.007 张永谦, 滕吉文, 王谦身, 等. 2013. 河套盆地及其邻近地域的地壳结构与深层动力学过程[J]. 地球物理学进展, 28(5): 2264−2272. 张玉清. 2004. 内蒙古白云鄂博北部宝音图岩群变质基性火山岩的年龄、构造背景及地质意义[J]. 地质通报, 23(2): 177−183. doi: 10.3969/j.issn.1671-2552.2004.02.012 张玉清, 苏宏伟. 2002. 内蒙古宝音图岩群变质基性火山岩锆石U−Pb年龄及意义[J]. 前寒武纪研究进展, 25(3/4): 199−204. 张允平, 苏养正, 李景春. 2010. 内蒙古中部地区晚志留世西别河组的区域构造学意义[J]. 地质通报, 29(11): 1599−1605. doi: 10.3969/j.issn.1671-2552.2010.11.001 章雨旭, 江少卿, 张绮玲, 等. 2008. 论内蒙古白云鄂博群和白云鄂博超大型稀土-铌-铁矿床成矿的年代[J]. 中国地质, 35(6): 1129−1137. doi: 10.3969/j.issn.1000-3657.2008.06.010 章雨旭, 柳建勇. 2010. 内蒙古达茂旗黑脑包腮林忽洞群中发现宏体化石[J]. 地质论评, 56(1): 123−124. 赵磊, 吴泰然, 罗红玲. 2011. 内蒙古乌拉特中旗北七哥陶辉长岩SHRIMP锆石U−Pb年龄、地球化学特征及其地质意义[J]. 岩石学报, 27(10): 3072−3081. 赵利刚, 李承东, 常青松, 等. 2016. 内蒙古白乃庙铜矿区含矿中酸性侵入岩LA−ICP−MS锆石U−Pb年龄、地球化学特征及成矿时代[J]. 地质通报, 35(4): 542−552. doi: 10.3969/j.issn.1671-2552.2016.04.008 赵利刚, 王文龙, 高学生, 等. 2024. 内蒙古达茂旗北部包尔汉图群时代及中早—中三叠世变质锆石年龄的启示[J]. 华北地质. 47(2): 1−16. 郑亚东, Davis G A, 王琮, 等. 1998. 内蒙古大青山大型逆冲推覆构造[J]. 中国科学(D辑), 28(4): 289−295. doi: 10.3321/j.issn:1006-9267.1998.04.001 郑永飞, 吴福元. 2009. 克拉通岩石圈的生长和再造[J]. 科学通报, 54: 1945−1949. 周建波, 郑永飞, 杨晓勇, 等. 2002. 白云鄂博地区构造格局与古板块构造演化[J]. 高校地质学报, 8(1): 46−61. doi: 10.3969/j.issn.1006-7493.2002.01.006 周志广, 张华锋, 刘还林, 等. 2009. 内蒙中部四子王旗地区基性侵入岩锆石定年及其意义[J]. 岩石学报, 25(6): 1519−1528. 周志广, 王果胜, 张达, 等. 2016. 内蒙古四子王旗地区侵入白云鄂博群辉长岩的年龄及其对白云鄂博群时代的约束[J]. 岩石学报, 32(6): 1809−1822. 周志广, 张达, 谷永昌, 等. 2018. 内蒙古白乃庙逆冲推覆构造特征及其地质意义[J]. 大地构造与成矿学, 42(1): 1−17. 朱日祥, 陈凌, 吴福元, 等. 2011. 华北克拉通破坏的时间、范围与机制[J]. 中国科学: 地球科学, 41: 583−592. 朱日祥, 徐义刚, 朱光, 等. 2012. 华北克拉通破坏[J]. 中国科学: 地球科学, 42(8): 1135−1159. 朱绅玉. 1997. 内蒙古色尔腾山—大青山地区推覆构造[J]. 内蒙古地质, 84(1): 41−47. 朱伟鹏, 田伟, 魏春景. 2023. 阴山东部固阳地区晚石炭世碱性火山岩的发现及其地质意义[J]. 岩石学报, 39(3): 670−688.
下载:
计量
- 文章访问数: 1303
- HTML全文浏览量: 269
- PDF下载量: 703
