Petrogenesis of Triassic granites in Xiaohongshan area, Beishan orogenic belt: Constraints from zircon U-Pb ages and Hf isotopes

LI Min; REN Bangfang; DUAN Xiaolong; TIAN Jian; DUAN Lianfeng; NIU Wenchao

Geological Bulletin of China > 2020 > 39(9): 1422-1435.

LI Min, REN Bangfang, DUAN Xiaolong, TIAN Jian, DUAN Lianfeng, NIU Wenchao. 2020: Petrogenesis of Triassic granites in Xiaohongshan area, Beishan orogenic belt: Constraints from zircon U-Pb ages and Hf isotopes. Geological Bulletin of China, 39(9): 1422-1435.

Citation:

PDF (8343 KB)

Petrogenesis of Triassic granites in Xiaohongshan area, Beishan orogenic belt: Constraints from zircon U-Pb ages and Hf isotopes

LI Min^{1, 2,},
REN Bangfang^{1, 2, ,},
DUAN Xiaolong^{1, 2},
TIAN Jian^{1, 2},
DUAN Lianfeng^{1, 2},
NIU Wenchao^{1, 2}

1.
Tianjin Center, China Geological Survey, Tianjian 300170, China
2.
North China Center for Geoscience Innovation, Tianjian 300170, China

More Information

Received Date: September 09, 2019
Revised Date: November 19, 2019
Available Online: August 15, 2023

Graphical Abstract

Abstract

Abstract

In this paper, zircon U-Pb ages, Hf isotopes and whole rock geochemical compositions of Triassic granite-porphyry in Xiaohongshan area of Beishan orogenic belt were systematically studied.Zircon LA-MC-ICP-MS U-Pb dating results show that the two ages of granite-porphyry are 211.8±1.6 Ma(the confidence value is 95%, n=24, MSDW=2.4)and 205.9±1.7 Ma(the confidence value is 95%, n=23, MSDW=2.9)respectively, which intruded at the late stage of Late Triassic.The granite-porphyry in the study area is characterized by high silicon, rich alkali, quasi-aluminum, and poor calcium, magnesium, and iron.It belongs to the series of high potassium calc-alkaline to potassic basanite with high degree of differentiation.It belongs to highly differentiated Ⅰ-type granite.It is enriched in Rb, Th, U, La, Ce and other large ion lithophile elements and depleted in Nb, P, Ti, Ba and Sr. It is characterized by low Sr, high Yb and Y with obvious negative europium anomaly.The ε_Hf(t)values range from -1.43 to 9.93, which are relatively high, and the Hf isotopic crustal model ages range from 610 Ma to 1335 Ma, indicating that the granite-porphyry was derived from the juvenile crust with mantle imprint mixed with remelting old crust. According to the data obtained in this paper and other regional geological data acquired recently, it is proposed that, under the post-orogenic extension system, the heat brought by the underplating of basic magma caused the partial melting of the juvenile crust from Neoproterozoic to Paleozoic, and suffered magma contamination of the remelting of the old crust of Lower Proterozoic.In addition, the magma was finally emplaced in the middle and upper crust after fractional crystallization, forming the the Late Triassic granite-porphyry in the study area.
- Triassic,
- granites,
- post-orogenic extension,
- zircon U-Pb age,
- zircon Hf isotopes,
- Beishan orogenic belt

FullText(HTML)

References (40)

References

Xiao W J, Mao Q G, Windley B F, et al.Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J].American Journal of Science, 2010, 310:1553-1594. doi: 10.2475/10.2010.12

Liu X C, Chen B, Jahn B M, et al.Early Paleozoic(ca.465 Ma)eclogites from Beishan(NW China)and their bearing on the tectonic evolution of the southern Central Asian Orogenic Belt[J].Journal of Asian Earth Sciences, 2011, 42(4):715-731. http://www.sciencedirect.com/science/article/pii/S1367912010003147

Guo Q Q, Xiao W J, Hou Q L, et al.Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt[J].Lithos, 2014, 184-187(1):361-378. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=12623046eb693c8acdf0846752adffb9

江思宏, 聂凤军.北山地区花岗岩类成因的Nd同位素制约[J].地质学报, 2006, 80(6):826-842. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200606005

Su B X, Qin K Z, Sun H, et al.Subduction-induced mantle heterogeneity beneath Eastern Tianshan and Beishan:Insights from Nd-Sr-Hf-O isotopic mapping of Late Paleozoic mafic-ultramafic complexes[J].Lithos, 2012, 134-135(2):41-51. http://www.sciencedirect.com/science/article/pii/S0024493711003847

Zhang W, Pease V, Wu T R, et al.Discovery of an adakite-like pluton near Dongqiyishan(Beishan, NW China)-Its age and tectonic significance[J].Lithos, 2012, 142-143(6):148-160. http://search.ebscohost.com/login.aspx?direct=true&db=aph&AN=75185132&site=ehost-live

Li S, Wilde S A, Wang T.Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China:Petrogenesis and tectonic implications[J].Lithos, 2013, 179:99-119. doi: 10.1016/j.lithos.2013.08.002

李敏, 任邦方, 滕学建, 等.内蒙古北山造山带花岗岩地球化学、锆石U-Pb年龄和Hf同位素特征及地质意义[J].地球科学, 2018, 43(12):4586-4605. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201812023

李敏, 辛后田, 任邦方, 等.内蒙古哈珠地区晚古生代花岗岩类成因及其构造意义[J].地球科学, 2019, 44(1):328-343. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201901023

潘志龙, 王硕, 邱振, 等.内蒙古北山地区咸水沟一带早石炭世红柳园组火山岩地球化学、锆石U-Pb年龄及Hf同位素特征[J].地质调查与研究, 2017, 40(02):99-108. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qhwjyjjz201702003

刘明强, 王建军, 代文军.甘肃北山红石山地区马鞍山北花岗岩体的单颗粒锆石U-Pb年龄及地质意义[J].岩石矿物学杂志, 2006, 25(6):473-479. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200606003

李舢, 王涛, 童英.中亚造山系中南段早中生代花岗岩类时空分布特征及构造环境[J].岩石矿物学杂志, 2010, 29(6):642-662. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201006004

Li S, Wang T, Wilde S A, et al.Geochronology, petrogenesis and tectonic implications of Triassic granitoids from Beishan, NW China[J].Lithos, 2012, 134-135:123-145. doi: 10.1016/j.lithos.2011.12.005

杨合群, 赵国斌, 李英, 等.新疆-甘肃-内蒙古衔接区古生代构造背景与成矿的关系[J].地质通报, 2012, 31(2/3):413-421. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2012020326&flag=1

Zuo G C, Zhang S L, He G Q, et al.Plate Tectonic characteristics during the Early Paleozoic in Beishan near the Sino-Mongolian Border Region, China[J].Tectonophysics, 1991, 188:385-392. doi: 10.1016/0040-1951(91)90466-6

耿建珍, 李怀坤, 张健, 等.锆石Hf同位素组成的LA-MC-ICP-MS测定[J].地质通报, 2011, 30(10):1508-1513. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20111004&flag=1

王树庆, 胡晓佳, 赵华雷.内蒙古苏左旗洪格尔地区新发现晚石炭世碱性花岗岩[J].地质调查与研究, 2019, 42(2):81-85. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qhwjyjjz201902001

Yuan H L, Gao S, Liu X M, et al.Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research, 2004, 28(3):353-370. doi: 10.1111/j.1751-908X.2004.tb00755.x

Liu Y S, Gao S, Hu Z C, et al.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J].J.Petrol., 2010, 51(1/2):537-571. http://petrology.oxfordjournals.org/content/51/1-2/537

Söderlund U, Patchett P J, Veroort J D, et al.The ¹⁷⁶Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Percambrian mafic intrusions[J].Earth and Planetary Science Letters, 2004, 219(3/4):311-324. http://www.sciencedirect.com/science/article/pii/S0012821X04000123

Bouvier A, Vervoort J D, Patchett P J.The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets[J].Earth and Planetary Science Letters, 2008, 273(1/2):48-57. http://www.sciencedirect.com/science/article/pii/S0012821X08003828

Griffin W L, Pearson N J, Elusive E, et al.The Hf isotopes composition of carbonic mantle:LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J].Geochim.Cosmochim.Acta, 2000, 64(1):133-147. doi: 10.1016/S0016-7037(99)00343-9

Griffin W L, Wang X, Jackson S E, et al.Zircon chemistry and magma mixing, SE China:in-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes[J]. Lithos, 2002, 61(3):237-269. http://www.sciencedirect.com/science/article/pii/S0024493702000828

Koschek G.Origin and significance of the SEM cathodoluminescence from zircon[J].Journal of Microscopy, 1993, 171(3):223-232. doi: 10.1111/j.1365-2818.1993.tb03379.x

Williams I S, Buick A, Cartwright I.An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynold region, central Australia[J].J.Metamorphic Geol., 1996, 14(1):29-47. doi: 10.1111/j.1525-1314.1996.00029.x

吴福元, 李献华, 郑永飞, 等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报, 2007, 23(2):185-220. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702001

Whalen J B, Currie K L, Chappell B W.A-Type granites:geochemical characteristics, discrimination and petrogenesis[J].Contrib.Mineral Petrol., 1987, 95:407-419. doi: 10.1007/BF00402202

刘昌实, 陈小明, 陈培荣, 等.A型岩套的分类、判别标志和成因[J].高校地质学报, 2003, 9(4):573-591. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200304011

Miller C F, McDowell S M, Mapes R W.Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance[J].Geology, 2003, 31:529-532. doi: 10.1130/0091-7613(2003)031<0529:HACGIO>2.0.CO;2

Ameilin Y, Lee D C, Halliiday A N, et al.Nature of the Earth's earliest crust from hafninm isotopes in single detrital zircon[J].Nature, 1999, 399(6733):252-255. doi: 10.1038/20426

Bleousova E A, Grifflin W L, O'Reilly S Y.Zircon crystal morphology, trace element signatures and Hf isotope composition as a tool for petrogenetic modelling:Examples from eastern Australian granitoids[J].Journal of Petrology, 2006, 47(2):329-353. doi: 10.1093/petrology/egi077

Kemp A I S, Hawkesworth C J, Foster G L, et al.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon[J].Science, 2007, 16:980-983. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=1dbf87dba7ccb9472238f299f960285c

Ravikant V, Wu F Y, Ji W Q, et al.U-Pb Age and Hf isotopic constraints of detrital zircons from the Himalayan foreland Subathu sub-basin on the Tertiary palaeogeography of the Himalaya[J].Earth and Planetary Science Letters, 2011, 304(3/4):356-368. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=fb603789424af69c5acd28427bf0aff8

Murphy J B, Nance R D.Sm-Nd isotopic systematics as tectonic tracers:an example from West Avalonia in the Canadian Appalachians[J].Earth-Science Reviews, 2002, 59(1/4):77-100. http://www.sciencedirect.com/science/article/pii/S0012825202000703

Kröner A, Kovach V, Belousova E, et al.Reassessment of continental growth during the accretionary history of the Central Asian Orogenie Belt[J].Gondwana Res., 2014, 25:103-125. http://www.sciencedirect.com/science/article/pii/S1342937X13000415

Jahn B M, Windley B, Natal'in B, et al.Phanerozoic Continental Growth in Central Asia[J].J.Asian Earth Sci., 2004, 23(5):599-603. doi: 10.1016/S1367-9120(03)00124-X

Windley B F, Alexeiev D, Xiao W J, et al.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of the Geological Society, 2007, 164:31-47. doi: 10.1144/0016-76492006-022

Sun M, Yuan C, Xiao W, et al.Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai:Progressive Accretionary history in the Early to Middle Palaeozoic[J].Chem.Geol., 2008, 247:352-383. https://ui.adsabs.harvard.edu/abs/2008ChGeo.247..352S/abstract

Wilhem C, Windley B F, Stampfli G M.The Altaids of Central Asia:A tectonic and evolutionary innovative review[J].Earth_Sci.Rev., 2012, 113:303-341. doi: 10.1016/j.earscirev.2012.04.001

Zong K Q, Klemd R, Yuan Y, et al.The assembly of Rodinia:The correlation of Early Neoproterozoic(ca.900 Ma)high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt(CAOB)[J].Precambrian Research, 2017, 290:32-48. doi: 10.1016/j.precamres.2016.12.010

Cited By

Get Citation

PDF

XML

Article views (2299) PDF downloads (1742)

Turn off MathJax

Article Contents

Abstract

References

	DENG Xianze, REN Jiangbo, DENG Xiguang, HE Gaowen, YANG Shengxiong. 2021: Cobalt-rich crust obtains high contents of key elements from seawater: element absorption and distribution. Geological Bulletin of China, 40(2-3): 376-384.
	LUO Shan, ZHANG Deming, LU Dingbiao, PENG Chenglong, AN Yayun, QIN Xingzhi. 2021: Evaluation of trace elements abundance and deficiency in cultivated soil and its influencing factors in Bijie City of Wumeng Mountain. Geological Bulletin of China, 40(9): 1570-1583.
	AN Yonglong, HUANG Yong, LIU Qingjun, SUN Chao, DENG Kaiwen, LI Di, HUANG Dan. 2016: The distribution of surface soil elements and the pollution assessment of heavy metal elements in Beijing. Geological Bulletin of China, 35(12): 2111-2120.
	CHEN Jian-fa, LU Jin-cai, TANG You-jun, WEI Jian-she, ZHU Lei, JIANG Ting, WANG Guan-nan. 2011: Abundance variation characteristics and hydrocarbon-generating potential of organic matter in Carboniferous-Permian dark argillaceous rock of Yingen-Ejin Banner basin, western Inner Mongolia. Geological Bulletin of China, 30(6): 859-864.
	CHEN Jian-fa, LU Jin-cai, SHI Zheng-yong, TANG You-jun. 2010: Development characteristics and hydrocarbon generating potential evolution of Permian-Carboniferous source rocks in Ejina Banner basin and its adjacent area, western Inner Mongolia, China. Geological Bulletin of China, 29(2-3): 346-350.
	XIONG Guo-qing, CAI Xi-yao, WU Hao, JIANG Xin-sheng. 2009: Organic matter abundance and significance of oil geology of the Cretaceous mudstones and shales from Rikaze area, southern Tibet, China. Geological Bulletin of China, 28(10): 1448-1457.
	LIU Hua, PENG Ping-an, LIU Da-yong, LIN Yu-xiang. 2006: Threshold of the organic matter abundance in marine carbonate source rocks in China. Geological Bulletin of China, 25(9): 1100-1103.
	WANG Yang. 2005: Comparison of element abundances between the exposed crust of the continent of China and the global average continental upper crust: Constraints on the crustal evolution and some speculations. Geological Bulletin of China, 24(10): 906-915.
	ZHANG Jisheng, HONG Dawei, WANG Tao. 2005: Gravity and magnetic field characteristics and density structure of the crust in central Inner Mongolia.. Geological Bulletin of China, 24(2): 118-123.
	Zhehuan ZHANG. 0: Soil geochemical baseline values and background values in Xunke Plain of HeiLongJiang Province. Geological Bulletin of China. DOI: 10.12097/gbc.2023.12.020

Petrogenesis of Triassic granites in Xiaohongshan area, Beishan orogenic belt: Constraints from zircon U-Pb ages and Hf isotopes

Abstract

References

Related Articles

Catalog

Petrogenesis of Triassic granites in Xiaohongshan area, Beishan orogenic belt: Constraints from zircon U-Pb ages and Hf isotopes

Abstract

References

Related Articles

Catalog

Export File

Citation

Format

Content