柴达木盆地北缘全吉群皱节山组碎屑锆石年代学特征及其地质意义

李猛; 王超; 李荣社; 彭岩; 邵东; 陈奋宁; 陈守建; 潘晓萍

doi:10.3799/dqkx.2018.106

Volume 43 Issue 12

Dec. 2018

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Article Navigation > Earth Science > 2018 > 43(12): 4390-4398

Li Meng, Wang Chao, Li Rongshe, Peng Yan, Shao Dong, Chen Fenning, Chen Shoujian, Pan Xiaoping, 2018. Detrital Zircon Geochronology and Geological Significance of Zhoujieshan Formation, Quanji Group in North Margin of Qaidam Basin. Earth Science, 43(12): 4390-4398. doi: 10.3799/dqkx.2018.106

Citation:

Li Meng, Wang Chao, Li Rongshe, Peng Yan, Shao Dong, Chen Fenning, Chen Shoujian, Pan Xiaoping, 2018. Detrital Zircon Geochronology and Geological Significance of Zhoujieshan Formation, Quanji Group in North Margin of Qaidam Basin. Earth Science, 43(12): 4390-4398. doi: 10.3799/dqkx.2018.106

Citation:

Li Meng, Wang Chao, Li Rongshe, Peng Yan, Shao Dong, Chen Fenning, Chen Shoujian, Pan Xiaoping, 2018. Detrital Zircon Geochronology and Geological Significance of Zhoujieshan Formation, Quanji Group in North Margin of Qaidam Basin. Earth Science, 43(12): 4390-4398. doi: 10.3799/dqkx.2018.106

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Detrital Zircon Geochronology and Geological Significance of Zhoujieshan Formation, Quanji Group in North Margin of Qaidam Basin

doi: 10.3799/dqkx.2018.106

1.
Xi'an Center of Geological Survey, Orogen Research Center, China Geological Survey, Xi'an 710054, China
2.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Xi'an 710054, China
3.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
4.
Institute of Geological Survey, Shaanxi Nuclear Industry, Xi'an 710100, China
5.
No.203 Research Institute of Nuclear Industry, Xianyang 712000, China

Received Date: 2018-05-29
Publish Date: 2018-12-15

Abstract

Abstract

The Quanji Group is mainly distributed in the north margin of Qaidam basin and consists of non-metamorphic sandstone, quartzite, sand shale, dolomite and tillite. U-Pb ages of detrital zircons from two sandstone samples in the Zhoujieshan Formation in the Upper Quanji Group were measured using the LA-ICP-MS method. The concordant ages of detrial zircons show that the provenance in the Zhoujieshan Formation was derived mainly from the Dakendaban Group of the Quanji block (1750-1990 Ma), subordinately from the Delingha complex (2 400-2 500 Ma). In addition, the detrital zircons record two important thermal events (~1.95 Ga and ~1.85 Ga) of the Quanji block in Paleoproterozoic-strong regional metamorphism and anatexis, with magmatic intrusion.
- Quanji Group,
- Zhoujieshan Formation,
- detrital zircon,
- zircon U-Pb age,
- Quanji block,
- geochemistry

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References(52)

References

Bureau of Geology and Mineral Resources of Qinghai Province, 1991.Regional Geology of Qinghai Province.Geological Publishing House, Beijing, 1-662 (in Chinese).

Chen, N.S., Gong, S.L., Sun, M., et al., 2009.Precambrian Evolution of the Quanji Block, Northeastern Margin of Tibet:Insights from Zircon U-Pb and Lu-Hf Isotope Compositions.Journal of Asian Earth Sciences, 35(3-4):367-376. doi: 10.1016/j.jseaes.2008.10.004

Chen, N.S., Gong, S.L., Xia, X.P., et al., 2013a.Zircon Hf Isotope of Yingfeng Rapakivi Granites from the Quanji Massif and 2.7 Ga Crustal Growth.Journal of Earth Science, 24(1):29-41. https://doi.org/10.1007/s12583-013-0309-2

Chen, N.S., Liao, F.X., Wang, L., et al., 2013b.Late Paleoproterozoic Multiple Metamorphic Events in the Quanji Massif:Links with Tarim and North China Cratons and Implications for Assembly of the Columbia Supercontinent.Precambrian Research, 228:102-116. https://doi.org/10.1016/j.precamres.2013.01.013

Chen, N.S., Zhang, L., Sun, M., et al., 2012.U-Pb and Hf Isotopic Compositions of Detrital Zircons from the Paragneisses of the Quanji Massif, NW China:Implications for Its Early Tectonic Evolutionary History.Journal of Asian Earth Sciences, 54-55:110-130. https://doi.org/10.1016/j.jseaes.2012.04.006

Gong, S.L., Chen, N.S., Wang, Q.Y., et al., 2012.Early Paleoproterozoic Magmatism in the Quanji Massif, Northeastern Margin of the Qinghai-Tibet Plateau and Its Tectonic Significance:LA-ICPMS U-Pb Zircon Geochronology and Geochemistry.Gondwana Research, 21(1):152-166. https://doi.org/10.1016/j.gr.2011.07.011

Hao, G.J., Lu, S.N., Wang, H.C., et al., 2004.The Pre-Devonian Tectonic Framework in the Northern Margin of Qaidam Basin and Geological Evolution of Olongbuluck Palaeo-Block.Earth Science Frontiers, 11(3):115-122 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200403016.htm

Li, H.K., Lu, S.N., Wang, H.C., et al., 2003.Quanji Group-The Geological Record of the Rodinia Supercontinent Break-up in the Early Neoproterozoic Preserved in the Northern Qaidam Margin, Qinghai, Northwest China.Geological Survey and Research, 26(1):27-37 (in Chinese with English abstract).

Li, X.Y., Chen, N.S., Xia, X.P., et al., 2007.Constraints on Timing of the Early-Paleoproterozoic Magmatism and Crustal Evolution of the Oulongbuluke Microcontinent:U-Pb and Lu-Hf Isotope Systematics of Zircons from Mohe Granitic Pluton.Acta Petrologica Sinica, 23(2):513-522 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200702028.htm

Liao, F.X., 2010.Chronology and Geochemistry of Delingha Metamorphosed Mafic Dyke Swarms (Dissertation).China University of Geosciences, Wuhan, 1-33(in Chinese).

Liu, Y.S., Gao, S., Hu, Z.C., et al., 2009.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 from Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571. https://doi.org/10.1093/petrology/egp082

Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004

Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4

Lu, S.N., Li, H.K., Zhang, C.L., et al., 2008.Geological and Geochronological Evidence for the Precambrian Evolution of the Tarim Craton and Surrounding Continental Fragments.Precambrian Research, 160(1-2):94-107. https://doi.org/10.1016/j.precamres.2007.04.025

Lu, S.N., Wang, H.C., Li, H.K., et al., 2002a.Redefinition of the "Dakendaban Group" on the Northern Margin of the Qaidam Basin.Geological Bulletin of China, 21(1):19-23 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200201003.htm

Lu, S.N., Yu, H.F., Zhao, F.Q., et al., 2002b.Preliminary Study of Precambrian Geology in the North Tibet-Qinghai Plateau.Geological Publishing House, Beijing, 1-125 (in Chinese).

Lu, S.N., Yu, H.F., Li, H.K., et al., 2006.Research on Precambrian Major Problems in China:Precambrian Important Geological Events in West China and Their Global Tectonic Significance.Geological Publishing House, Beijing, 1-206 (in Chinese).

Ludwig, K.R., 2003.Isoplot 3.0-A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication, Berkeley.

Shen, B., Xiao, S.H., Dong, L., et al., 2007.Problematic Macrofossils from Ediacaran Successions in the North China and Chaidam Blocks:Implications for Their Evolutionary Roots and Biostratigraphic Significance.Journal of Paleontology, 81(6):1396-1411. https://doi.org/10.1666/06-016r.1

Shen, B., Xiao, S.H., Zhou, C.M., et al., 2010.Carbon and Sulfur Isotope Chemostratigraphy of the Neoproterozoic Quanji Group of the Chaidam Basin, NW China:Basin Stratification in the Aftermath of an Ediacaran Glaciation Postdating the Shuram Event?.Precambrian Research, 177(3-4):241-252. https://doi.org/10.1016/j.precamres.2009.12.006

Sun, C.R., Chen, G.L., Li, Z.R., et al., 1997.Multiple Classification and Correlation of the Stratigraphy of China(63):Stratigraphy (Lithostratic) of Qinghai Province.China University of Geosciences Press, Wuhan, 1-340 (in Chinese).

Wang, C., Li, M., Li, R.S., et al., 2015.Recognition of the Regional Unconformity in the Neoproterozoic Quanji Group on the North Margin of the Qaidam Basin in Qinghai Province.Geological Bulletin of China, 34(2-3):364-373 (in Chinese with English abstract).

Wang, C., Li, R.S., Li, M., et al., 2015.Palaeoproterozoic Magmatic-Metamorphic History of the Quanji Massif, Northwest China:Implications for a Single North China-Quanji-Tarim Craton within the Columbia Supercontinent? International Geology Review, 57(13):1772-1790. https://doi.org/10.1080/00206814.2015.1026849

Wang, C., Liu, L., Li, R.S., 2018.Precambrian Geology of the Northern Margin of the Tibetan Plateau:Review and Discussion.Chinese Journal of Geology, 53(3):1-28(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dzkx201803012

Wang, Q.Y., Chen, N.S., Li, X.Y., et al., 2008.LA-ICPMS U-Pb Dating for the Basement Dakendaban Group and Thermal Event in Quanji Block.Chinese Science Bulletin, 53 (14):1693-1701(in Chinese).

Wang, Q.Y., Pan, Y.M., Chen, N.S., et al., 2009.Proterozoic Polymetamorphism in the Quanji Block, Northwestern China:Evidence from Microtextures, Garnet Compositions and Monazite CHIME Ages.Journal of Asian Earth Sciences, 34(5):686-698. https://doi.org/10.1016/j.jseaes.2008.10.008

Wang, S.X., 1982.Stromatolite from Quanji Group in Qinghai Province and Its Stratigraphic Significance.Northwestern Geology, 15(4):1-10, 72-73 (in Chinese).

Wang, Y.S., Zhuang, Q.X., Shi, C.Y., et al., 1980.Quanji Group along the Northern Border of Chaidamu Basin.In: Tianjin Institute of Geology and Mineral Resources, CAGS, ed., Research on Precambrian Geology: Sinian Suberathem in China.Tianjin Science and Technology Press, Tianjin, 214-230 (in Chinese).

Zhang, H.J., Wang, X.L., Wang, X., et al., 2016.U-Pb Zircon Ages of Tuff Beds from the Hongzaoshan Formation of the Quanji Group in the North Margin of the Qaidam Basin, NW China, and Their Geological Significances.Earth Science Frontiers, 23(6):202-218 (in Chinese).

Zhang, J.X., Wan, Y.S., Xu, Z.Q., et al., 2001.Discovery of Basic Granulite and Its Formation Age in Delingha Area, North Qaidam Mountains.Acta Petrologica Sinica, 17(3):453-458(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200103013.htm

Zhang, L., 2014.Petrogenesis of the (Meta-) Precambrian Clastic Sedimentary Rocks from the Quanji Massif, Northwestern China and Tectonic Implications (Dissertation).China University of Geosciences, Wuhan, 1-127 (in Chinese).

Zhang, L., Ba, J., Chen, N.S., et al., 2012.U-Pb Age Spectra and Trace Elements of Detrital Zircon from Quanji Group:Implications for Thermal Events and Early Evolution in the Basement.Earth Science, 37(S1):28-42 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2012.S1.004

Zhang, L., Liao, F.X., Ba, J., et al., 2011.Mineral Evolution and Zircon Geochronology of Mafic Enclave in Granitic Gneiss of the Quanji Block and Implications for Paleoproterozoic Regional Metamorphism.Earth Science Frontiers, 18(2):79-84 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201102007

青海省地质矿产局, 1991.青海省区域地质志.北京:地质出版社, 1-662.

郝国杰, 陆松年, 王惠初, 等, 2004.柴达木盆地北缘前泥盆纪构造格架及欧龙布鲁克古陆块地质演化.地学前缘, 11(3):115-122. doi: 10.3321/j.issn:1005-2321.2004.03.013

李怀坤, 陆松年, 王惠初, 等, 2003.青海柴北缘新元古代超大陆裂解的地质记录——全吉群.地质调查与研究, 26(1):27-37. doi: 10.3969/j.issn.1672-4135.2003.01.006

李晓彦, 陈能松, 夏小平, 等, 2007.莫河花岗岩的锆石U-Pb和Lu-Hf同位素研究:柴北欧龙布鲁克微陆块始古元古代岩浆作用年龄和地壳演化约束.岩石学报, 23(2):513-522. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702027

廖梵汐, 2010.德令哈变质镁铁质岩墙群的年代学和地球化学研究(学士学位论文).武汉: 中国地质大学, 1-33.

陆松年, 王惠初, 李怀坤, 等, 2002a.柴达木盆地北缘"达肯大坂群"的再厘定.地质通报, 21(1):19-23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200201004

陆松年, 于海峰, 赵凤清, 等, 2002b.青藏高原北部前寒武纪地质初探.北京:地质出版社, 1-125.

陆松年, 于海峰, 李怀坤, 等, 2006.中国前寒武纪重大地质问题研究——中国西部前寒武纪重大地质事件群及全球构造意义.北京:地质出版社, 1-206.

孙崇仁, 陈国隆, 李璋荣, 等, 1997.青海省岩石地层.武汉:中国地质大学出版社, 1-340.

王超, 李猛, 李荣社, 等, 2015.青海柴达木盆地北缘全吉群内部存在区域性不整合.地质通报, 34(2-3):364-373. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201502014

王超, 刘良, 李荣社, 2018.青藏高原北缘前寒武纪地质演化:进展与讨论.地质科学, 53(3):1-28. http://d.old.wanfangdata.com.cn/Periodical/dzkx201803012

王勤燕, 陈能松, 李晓彦, 等, 2008.全吉地块基底达肯大坂岩群和热事件的LA-ICPMS锆石U-Pb定年.科学通报, 53(14):1693-1701. doi: 10.3321/j.issn:0023-074X.2008.14.010

王树洗, 1982.青海全吉群的几个叠层石群及其地层意义.西北地质, 15(4):1-10, 72-73. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDI198204000.htm

王云山, 庄庆兴, 史从彦, 等, 1980.柴达木北缘的全吉群.见: 中国地质科学院天津地质矿产研究所编, 中国震旦亚界.天津: 天津科学技术出版社, 214-230.

张海军, 王训练, 王勋, 等, 2016.柴达木盆地北缘全吉群红藻山组凝灰岩锆石U-Pb年龄及其地质意义.地学前缘, 23(6):202-218. http://d.old.wanfangdata.com.cn/Periodical/dxqy201606014

张建新, 万渝生, 许志琴, 等, 2001.柴达木北缘德令哈地区基性麻粒岩的发现及其形成时代创.岩石学报, 17(3):453-458. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200103014

张璐, 2014.全吉地块元古代(变)沉积碎屑岩的成因和构造演化(博士学位论文).武汉: 中国地质大学, 1-127.

张璐, 巴金, 陈能松, 等, 2012.全吉群碎屑锆石的U-Pb年龄谱和微量元素:基底热事件信息和早期演化启示.地球科学, 37(S1):28-42. http://d.old.wanfangdata.com.cn/Periodical/dqkx2012z1004

张璐, 廖梵汐, 巴金, 等, 2011.全吉地块花岗片麻岩中镁铁质岩包体的矿物演化和锆石定年与古元古代区域变质作用.地学前缘, 18(2):79-84. http://d.old.wanfangdata.com.cn/Periodical/dxqy201102007

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Detrital Zircon Geochronology and Geological Significance of Zhoujieshan Formation, Quanji Group in North Margin of Qaidam Basin

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