| Citation: |
Shao Z G, Chen X H, Wang Z Z, Chen Y F, Xu S L, Yu W, Su H, Han L L, Xu D X, Ding Y W. Characteristics of Heiyingshan Late Triassic thrust nappe structure in the Beishan orogenic belt and its constraint on the evolution of the orogenic belt. Geological Bulletin of China, 2024, 43(11): 1893−1906. DOI: 10.12097/gbc.2024.03.033
|
Beishan orogenic belt is located in the southern margin of the Central Asian tectonic belt, where the Tarim Plate, North China Plate and Siberia Plate meet, which is the most significant area of the Phanerozoic continental crust accretion and transformation in the world, has become the key area for studying the process from subduction to final collage closure and intracontinental transformation of the Paleo−Asian Ocean, and the process of intracontinental transformation covers the complex process of intracontinental deformation, basin-mountain coupling and readjusting since Late Paleozoic, especially during the Mesozoic and Cenozoic. Previous studies on the Beishan orogenic belt mainly focus on the early subduction and collision process, but the study on the intracontinental stage, especially the Indosinian tectonic process is relatively weak. In the field geological survey of the Heiyingshan area in the northern of the Beishan orogenic belt, we found the Early Paleozoic metamorphic sandstone-volcanic rocks thrust southward onto the carboniferous andesitic volcanic tuff and Triassic acid fused tuff, metamorphic sandstone. By studying the structural characteristics of the thrust system and the zircon U−Pb ages of the upper and lower strata volcanic rocks, it is proposed that the thrust system has nappe from north to south and shows the characteristics of the ‘flyover type’ superimposed structure. The new geochronological data indicate that the thrust nappe system is the result of intracontinental compression in Beishan orogenic belt during the Late Triassic (Late Indosinian). The identification and age determination of the Heiyingshan thrust nappe structure have important significance for a further understanding of the intracontinental tectonic evolution of the Beishan orogenic belt.
|
Charvet J, Shu L, Laurent-Charvet S. 2007. Paleozoic structural and geodynamic evolution of eastern Tianshan (NW China): welding of the Tarim and Junggar plates[J]. Episodes, 30: 162−185.
|
|
Chen Z B, Yu Y, Bo H J. 2020. Geochemical Characteristics and Geological Significance of the Ordovician Volcanic Rock in Ejiana, Inner Mongolia[J]. Earth Science, 45(2): 503−518 (in Chinese with English abstract).
|
|
Corfu F, Hanchar J M, Hoskin P W O, et al. 2003. Altas of zircon textures[J]. Reviews in Mineralogy & Geochemistry, 53(1): 469−500.
|
|
Ding J X, Han C M, Xiao W J, et al. 2015. Geochemistry and U-Pb geochronology of tungsten deposit of Huaniushan island arc in the Beishan Orogenic Belt, and its geodynamic background[J]. Acta Petrologica Sinica, 31(2): 594−616 (in Chinese with English abstract).
|
|
Dong Z C, Xi R G, Wang G Q, et al. 2024. Structural characteristics of the Saozishan Formation in the Hongshishan area of the Gansu Beishan and its dynamic background[J]. Geological Bulletin of China, 43(2/3): 302−316 (in Chinese with English abstract).
|
|
Gong Q S, Liu M L, Liang M H, et al. 2003. The tectonic facies and tectonic evolution of Beishan orogenic belt, Gansu[J]. Northwestern Geology, 36(1): 11−17 (in Chinese with English abstract).
|
|
Jahn B M. 2004. The Cental Asian Orogenic Belt and growth of the continental crust in the Phanerozoic[J]. Geological Society Special Pulication, 226: 73−100. doi: 10.1144/GSL.SP.2004.226.01.05
|
|
Ludwig K R. 2003. User’s Manual for Isoplot 3.0: A Geochronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Center. Special publication, 4: 1−71.
|
|
Niu W C, Xin H T, Duan L F, et al. 2020. Geochemical characteristics, zircon U-Pb age of SSZ ophiolite in the Baiheshan area of the Beishan orogenic belt, Inner Mongolia, and its indication for the evolution of the Paleo-Asian Ocean[J]. Geological Bulletin of China, 39(9): 1317−1329 (in Chinese with English abstract).
|
|
Soldner J, Yuan C, Schulmann K, et al. 2020. Grenvillean evolution of the Beishan Orogen, NW China: Implications for development of an active Rodinian margin[J]. The Geological Socity of America, 132(7/8): 1657−1680.
|
|
Song B, Zhang Y H, Wan Y S, et al. 2002. Mount making and procedure of the SHRIMP dating[J]. Geological Review, 48(S1): 26−30 (in Chinese with English abstract).
|
|
Song D F, Xiao W J, Han C M, et al. 2013a. Progressive accretionary tectonics of the Beishan orogenic collage, southern Altaids: 1551 Insights from zircon U-Pb and Hf isotopic data of high-grade complexes[J]. Precambrian Research, 227: 368−388. doi: 10.1016/j.precamres.2012.06.011
|
|
Song D F, Xiao W J, Han C M, et al. 2013b. Geochronological and geochemical study of gneiss-schist complexes and associated granitoids, Beishan Orogen, southern Altaids[J]. International Geology Review, 55(14): 1705−1727. doi: 10.1080/00206814.2013.792515
|
|
Su B X, Qin K Q, Sakyi A, et al. 2011. Geochemistry and geochronology of acidic rocks in the Beishan region, NW China: Petrogenesis and tectonic implications[J]. Journal of Asian Earth Sciences, 41: 31−43. doi: 10.1016/j.jseaes.2010.12.002
|
|
Tang K D, Yan Z Y. 1993. Regional metamorphism and tectonic evolution of the Inner Mongolian suture zone[J]. Journal of Metamorphic Geology, 11: 511−522.
|
|
Wang B, Chen Y, Zhan S, et al. 2007. Primary Carboniferous and Permian paleomagnetic results from the Yili Block (NW China) and their implications on the geodynamic evolution of Chinese Tianshan Belt[J]. Earth and Planetary Science Letters, 263: 288−308. doi: 10.1016/j.jpgl.2007.08.037
|
|
Wang G Q, Li X M, Xu X Y, et al. 2014. Ziron U-Pb chronological study of the Hongshishan ophiolite in the Beishan area and their tectonic significance[J]. Acta Petrologica Sinica, 30(6): 1685−1694 (in Chinese with English abstract).
|
|
Wei Y S, Yan T, Yang W B, et al. 2020. The establishment of Late Paleozoic stratigraphic framework in the northern belt of Beishan orogenic belt of Inner Mongolia[J]. Geological Bulletin of China, 39(9): 1367−1388 (in Chinese with English abstract).
|
|
Windley B F, Dmitriy A, Xiao W J, et al. 2007. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 164: 31−47. doi: 10.1144/0016-76492006-022
|
|
Wu P, Wang G Q, Li X M, et al. 2012. The age of Niujuanzi ophiolite in Beishan area of Gansu Province and its geological significance[J]. Geological Bulletin of China, 31(12): 2032−2037 (in Chinese with English abstract) .
|
|
Wu Y D, Zheng Y F. 2004. Genesis of zircon and its constraints on interpretation of U-Pb age[J]. Chinese Science Bulletin, 49(15): 1553−1569.
|
|
Xiao W J, Windley B F, Yuan C, et al. 2009. Paleozoic multiple subduction-accretion processes of the southern Altaids[J]. American Journal of Science, 309: 221−270. doi: 10.2475/03.2009.02
|
|
Xiao W J, Mao Q G, Windley B F, et al. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310: 1553−1594. doi: 10.2475/10.2010.12
|
|
Xiao W J, Santosh M. 2015. Continental reconstruction and metallogeny of the Circum-Junggar areas and termination of the southern Central Asian Orogenic Belt[J]. Geoscience Frontiers, 6: 137−140. doi: 10.1016/j.gsf.2014.11.003
|
|
Xie C L, Yang J G, Wang L S, et al. 2009. Disscussion on the location of Paleozoic island arc zone on the south margin of Paleo-Asian Ocean in the Beishan[J]. Acta Geologica Sinica, 83(11): 1584−1600 (in Chinese with English abstract).
|
|
Yu C, Yang Z M, Zhou L M, et al. 2019. Impact of laser focus on accuracy of U-Pb dating of zircons by LA-ICPMS[J]. Mineral Deposits, 38(1): 21−28 (in Chinese with English abstract).
|
|
Yue Y, Liou J G, Graham S A. 2001. Tectonic correlation of Beishan and Inner Mongolia orogens and its implications for the palinspastic reconstruction of north China[C]// Hendrix M S, Davis G A. Paleozoic and Mesozoic tectonic evolution of Central and Eastern Asia: from continental assembly to intracontinental deformation. Geological Society of America Memoir, 194: 101−116.
|
|
Zhang J, Cunningham D. 2012. Kilometer-scale refolded folds caused by strike-slip reversal and intraplate shortening in the Beishan region, China[J]. Tectonics, 31: TC3009.
|
|
Zhang W, Pease V, Meng Q P, et al. 2015. Timing, petrogenesis and setting of granites from the southern Beishan late Palaeozoic granitic belt, Northwest China and implications for their tectonic evolution[J]. International Geology Review, 57(16): 1975−1991. doi: 10.1080/00206814.2015.1045944
|
|
Zhang Y L, Xu R K, Shan L, et al. 2012. Rock-forming and ore-forming ages of the Xiaohulishan molybdenum deposit in Beishan area, Inner Mongolia[J]. Geological Bulletin of China, 31(2/3): 469−475 (in Chinese with English abstract).
|
|
Zheng Y D, Zhang Y, Wang Y, et al. 1996. Great Jurassic thrust sheets in Beishan (North Mountains) −Gobi areas of China and southern Mongolia[J]. Journal of Structural Geology, 18: 1111−1126. doi: 10.1016/0191-8141(96)00038-7
|
|
Zuo G C, Zhang S L, He G Q, et al. 1991. Plate tectonic characteristics during the early Paleozoic in Beishan near the Sino-Mongolian border region, China[J]. Tectonophysics, 188: 385−392. doi: 10.1016/0040-1951(91)90466-6
|
|
Zuo G C, Feng Y Z, Liu C Y, et al. 1992. A new discovery of Early Yanshanian strike-slip compressional nappe zones on middle-southern segment of Beishan MTS, Gansu[J]. Scientia geological sinica, (4): 309−316 (in Chinese with English abstract).
|
|
陈智斌, 于洋, 薄海军. 2020. 内蒙古额济纳地区奥陶纪火山岩地球化学特征及其地质意义[J]. 地球科学, 45(2): 503−518.
|
|
董增产, 奚仁刚, 王国强, 等. 2024. 甘肃北山红石山地区扫子山组构造变形特征及其动力学背景[J]. 地质通报, 43(2/3): 302−316.
|
|
丁嘉鑫, 韩春明, 肖文交, 等. 2015. 北山造山带花牛山岛弧东段钨矿床成矿时代和成矿动力学过程[J]. 岩石学报, 31(2): 594−616.
|
|
龚全胜, 刘明强, 梁明宏, 等. 2003. 北山造山带大地构造相及构造演化[J]. 西北地质, 36(1): 11−17. doi: 10.3969/j.issn.1009-6248.2003.01.002
|
|
牛文超, 辛后田, 段连峰, 等. 2020. 内蒙古北山造山带百合山SSZ型蛇绿岩地球化学特征、锆石U-Pb年龄及其对古亚洲洋演化的指示[J]. 地质通报, 39(9): 1317−1329.
|
|
宋彪, 张玉海, 万渝生, 等. 2002. 锆石SHRIMP样品靶制作、年龄测定及有关现象讨论[J]. 地质论评, 48(S1): 26−30.
|
|
王国强, 李向民, 徐学义, 等. 2014. 甘肃北山红石山蛇绿岩锆石U-Pb年代学研究及构造意义[J]. 岩石学报, 30(6): 1685−1694.
|
|
卫彦升, 闫涛, 杨五宝, 等. 2020. 内蒙古北山造山带北带晚古生代地层时空格架的建立[J]. 地质通报, 39(9): 1367−1388.
|
|
武鹏, 王国强, 李向民, 等. 2012. 甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义[J]. 地质通报, 31(12): 2032−2037.
|
|
谢春林, 杨建国, 王立社, 等. 2009. 甘肃北山地区古亚洲南缘古生代岛弧带位置的讨论[J]. 地质学报, 83(11): 1584−1600.
|
|
于超, 杨志明, 周利敏, 等. 2019. 激光焦平面变化对LA-ICPMS锆石U-Pb定年准确度的影响[J]. 矿床地质, 38(1): 21−28.
|
|
张雨莲, 许荣科, 陕亮, 等. 2012. 内蒙古北山地区小狐狸山钼矿辉钼矿Re-Os年龄和LA-ICP-MS锆石U-Pb年龄[J]. 地质通报, 31(2/3): 469−475. doi: 10.3969/j.issn.1671-2552.2012.02.033
|
|
左国朝, 冯永忠, 刘春燕, 等. 1992. 甘蒙北山中南带新发现燕山早期走滑挤压推覆构造带[J]. 地质科学, (4): 309−316.
|
| 1. |
李林，曾磊，董英，张戈，朱立峰. 基于三维地质模型的西咸新区地下空间开发适宜性评价. 地质与勘探. 2024(01): 197-206 .
| |
| 2. |
贾伍慧，李宗发，刘凯，闫金凯，朱伟，郭本力，杨鹏. 典型滨海平原城市地下空间地质适宜性评价. 地质与勘探. 2024(02): 367-376 .
| |
| 3. |
宋云丽，严云籍，翟林博，吴白玉，姚佳其，何海龙. 抽水蓄能电站建设的地理要素分析及GIS选址. 云南水力发电. 2022(04): 131-134 .
| |
| 4. |
郑明贵，吴萍，尤碧莹. 中国铁矿资源经济安全评价与预警. 地质通报. 2022(05): 836-845 .
本站查看
|
Supported by: Beijing Renhe Information Technology Co., Ltd. 
DownLoad: