羌塘-三江古生代-中生代沉积盆地演化

孔令耀; 姚华舟; 徐亚东; 骆满生; 罗亮; 吴旌

doi:10.3799/dqkx.2014.105

Volume 39 Issue 8

Aug. 2014

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2014 > 39(8): 1217-1229

Kong Lingyao, Yao Huazhou, Xu Yadong, Luo Mansheng, Luo Liang, Wu Jing, 2014. Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic. Earth Science, 39(8): 1217-1229. doi: 10.3799/dqkx.2014.105

Citation:

Kong Lingyao, Yao Huazhou, Xu Yadong, Luo Mansheng, Luo Liang, Wu Jing, 2014. Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic. Earth Science, 39(8): 1217-1229. doi: 10.3799/dqkx.2014.105

Citation:

PDF( 3339 KB)

Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic

doi: 10.3799/dqkx.2014.105

Kong Lingyao^{1, 2
,},
Yao Huazhou^{2
,
,},
Xu Yadong^{3, 4},
Luo Mansheng³,
Luo Liang⁵,
Wu Jing⁴

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Wuhan Center of China Geological Survey, Wuhan 430205, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
4.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
5.
Chengdu Center of China Geological Survey, Chengdu 610082, China

Received Date: 2014-06-05
Publish Date: 2014-08-01

Abstract

Abstract

The structure and evolution of Qiangtang-Sanjiang during Paleozoic-Mesozoic sedimentary basins were controlled by the Tethys. On the basis of the exploration of previous studies on lithostratigraphy, fossil assemblages, isotopic geochronology and tectonics of the study area, this paper classifies the sedimentary basins of Qiangtang-Sanjiang region, and analyzes the formation and evolution of each sedimentary basin. During the Early Paleozoic, Qiangtang-Sanjiang basins were mostly ocean environment; with the subduction of the Tethys Ocean to the northeastward and southeastward in Late Paleozoic, the active margin sedimentary basins developed in this area, forming Jinshajiang back arc-ocean, Lancangjiang back arc-ocean and Ganzi-Litang back arc-ocean and then the multiple island arc-basin systems of eastern Tethys system gradually formed. During the Mesozoic, with the subduction of the Tethys in Late Triassic in Qiangtang-Sanjiang, three arc-basins gradually closed, then large-scale arc-arc collision and arc-continent collision occurred in this area. This area eventually entered intracontinental evolution stage from the active margin sedimentary basins, Due to the close of Tethys in Cretaceous, the Indian plate and western China collided, inland basins developed in Qiangtang-Sanjiang.
- Qiangtang-Sanjiang,
- active continental margin,
- Tethys,
- sedimentology,
- tectonics,
- basin evolution

FullText(HTML)

References(103)

References

Chen, L., Yin, H.S., Shi, Z.Q., 2002. The Jurassic Sediments and Their Depositional Environments in the Yanshiping Region of the Qiangtang Basin, Northern Xizang. Sedimentary Geology and Tethyan Geology, 22(3): 80-84 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD200203012.htm

Chen, M., Luo, J.N., 1999. Sedimentary Characteristics and Evolution of the Yidun Foreland Basin, Western Sichuan during the Early-Late Triassic. Sedimentary Geology and Tethyan Geology, 23: 108-120 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD199900011.htm

Chen, S.J., Li, R.S., Ji, W.H., et al., 2011. Lithostratigraphy Character and Tectonic-Evolvement of Permian-Trias in the Bayankala Tectonic Belt. Earth Science—Journal of China University of Geosciences, 36(3): 393-408 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_earth-science_thesis/0201252995438.html

Dai, Z.M., Sun, C.M., 2008. Evolution of Triassic Volcanic-Sedimentary Basins in the Central Segment of the Yidun Island Arc of the Songpan-Garzê Orogenic Belt, Western Sichuan, China. Geological Bulletin of China, 27(6): 799-813 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-ZQYD200806010.htm

Feng, Q.L., Ye, M., Zhang, Z.J., 1997. Early Carboniferous Radiolarians from Western Yunnan. Acta Micropalaeontologica Sinica, 14(1): 79-92 (in Chinese).

Fu, X.G., Wang, J., Tan, F.W., et al., 2009a. Zircon SHRIMP U-Pb Age of Volcanic Rocks in E'erlongba Formation, Eastern Part of the Qiangtang Basin, Qinghai-Tibet Plateau, China and Its Geological Significance. Geological Bulletin of China, 28(5): 561-567(in Chinese with English abstract). http://www.researchgate.net/publication/296067404_Zircon_SHRIMP_U-Pb_age_of_volcanic_rocks_in_E'er-longba_Formation_eastern_part_of_the_Qiangtang_basin_Qinghai-Tibet_Plateau_China_and_its_geological_significance

Fu, X.G., Wang, J., Wu, T., 2009b. Discovery of the Large-Scale Paleo-Weathering Crust in the Qiangtang Basin, Northern Tibet, China and Its Significance. Geological Bulletin of China, 28(6): 696-700 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-bulletin-china_thesis/0201252286383.html

Gou, J., 1990. The Basic Features of Ultrabasic Rocks in Bayinchawuma, Tanggula. Northwestern Geology, (1): 1-5(in Chinese).

Jia, J.C., Wu, X.G., Wang, H.G., et al., 2006. Mesozoic Sedimentary Characteristics and Tectonic Evolution in the Eastern Part of the Qiangtang Basin. Geology in China, 33(5): 999-1004 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200605008.htm

Jian, P., Liu, D.Y., Zhang, Q., et al., 2003. SHRIMP U-Pb Dating of Ophiolites and Leucocratic Rocks within Ophiolites. Earth Science Frontiers, 10(4): 439-456(in Chinese with English abstract). http://www.researchgate.net/publication/281201195_SHRIMP_dating_of_ophiolite_and_leucocratic_rocks_within_ophiolite

Jian, P., Wang, X.F., He, L.Q., 1998. Geochronology of Ophiolitic Rocks from the Ailaoshan Suture, Yunnan Province, Southwestern China: Implications of Palaeothyan Evolution. Geology and Mineral Resources of South China, (1): 1-11 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HNKC199801000.htm

Kou, L.L., Zhong, K.H., Tang, J.X., et al., 2009. Geochemistry Discrimination of Late Triassic Volcanic Rocks in Changdu-Simao Tectonic Zone. Northwestern Geology, 42(1): 79-87 (in Chinese with English abstract). http://www.researchgate.net/publication/287894471_Geochemistry_discrimination_of_late_Triassic_volcanic_rocks_in_Changdu-Simao_Tectonic_zone

Lei, D.J., 1987. The Cognition of Major Active Fault Zones in the West of Lancangjiang. Yunan Geology, 6(2): 188-196 (in Chinese).

Li, B.Q., Yao, J.X., Gao, L.D., et al., 2007. Age and Source Regions of the Wenquangou Group in the Mazar-Kangxiwar Area, West Kunlun Mountains. Geological Bulletin of China, 26(4): 457-465 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/zgqydz200704012

Li, Y., Hou, M.C., Kang, K., et al., 2013. Sedimentary Environments of the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar Block, Western Kunlun Mountains. Sedimentary Geology and Tethyan Geology, 33(1): 55-61 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD201301010.htm

Li, Y., Wang, C.S., Yi, H.S., 2002. Filled Sequence and Evolution of the Mesozoic Qiangtang Composite Foreland Basin in the Qinghai-Tibet Plateau. Journal of Stratigraphy, 26(1): 62-79 (in Chinese with English abstract). http://www.researchgate.net/publication/285079604_Filled_sequence_and_evolution_of_the_Mesozoic_Qiangtang_composite_foreland_hasin_in_the_Qinghai-Tibet_Plateau

Li, Y., Wang, C.S., Yi, H.S., 2003. The Late Triassic Collision and Sedimentary Responses at Western Segment of Jinshajiang Suture, Tibet. Acta Sedimentologica Sinica, 21(2): 191-197 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=7880994

Liang, B., Feng, Q.L., Wang, Q.W., et al., 2004. The Tectonic Evolution of the Ladinian Radiolarian and Siliceous in Xianshui River of West Sichuan Province. Science in China(Ser. D), 34(7): 644-648 (in Chinese).

Liang, B., Yang, F.Q., Guo, J.Q., et al., 2003. Discovery of Deep Water Trace Fossils from Late Triassic Yajiang Formation and Lianghekou Formation in Yajiang County, Sichuan Province. Geological Science and Technology Information, 22(3): 41-44(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200303008.htm

Mi, Y.C., Fang, P.Y., Hu, Y.X., et al., 2012. The Division and Evolution of Tectonic Unit in Changdu-Puer Massif of Mid Sector of Lancangjiang River. Yunnan Geology, 32(4): 512-515(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YNZD201204024.htm

Mo, X.X., Pan, G.T., 2006. From the Tethys to the Formation of the Qinghai-Tibet Plateau: Constrained by Tectono-Magmatic Events. Earth Science Frontiers, 13(6): 43-51 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy200606007

Pan, G.T., Wang, L.Q., Li, R.S., et al., 2012. Tectonic Model of Archipelagic Arc-Basin Systems: The Key to the Continental Geology. Sedimentary Geology and Tethyan Geology, 32(3): 1-20(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_sedimentary-geology-tethyan_thesis/0201252083843.html

Pan, G.T., Wang, L.Q., Zhang, W.P., et al., 2013. The Instructions of Tectonic Map in Qinghai-Tibet Plateau and Its Adjacent Areas (1∶1 500 000). Chengdu Cartographic Publishing House, Chengdu(in Chinese).

Pan, G.T., Xiao, Q.H., Lu, S.N., et al., 2009. Subdivision of Tectonic Units in China. Geology in China, 36(1): 1-28 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200901004.htm

Peng, D., Lin, L., Wang, Q.W., et al., 2011. The Discovery of Manganese Nodules in Garze-Litang Suture Zone. Geology in China, 38(2): 442-450 (in Chinese with English abstract). http://www.researchgate.net/publication/287680680_The_discovery_of_manganese_nodules_in_Garze-Litang_suture_zone

Peng, X.J., Luo, W.L., 1982. A Preliminary Identification of the Paired Metamorphic Zones in the Southern Segment of Lancangjiang. The Tibetan Plateau Geological Collected Works, (13): 21-30 (in Chinese with English abstract).

She, H.Q., Li, J.W., Ma, D.F., et al., 2009. Molybdenite Re-Os and SHRIMP Zircon U-Pb Dating of Duobuza Porphyry Copper Deposit in Tibet and Its Geological Implications. Mineral Deposits, 28(6): 737-746 (in Chinese with English abstract). http://www.researchgate.net/publication/283432285_Molybdenite_Re-Os_and_SHRIMP_zircon_U-Pb_dating_of_Duobuza_porphyry_copper_deposit_in_Tibet_and_its_geological_implications

Wang, E., Wan, J., Liu, J., 2003. Late Cenozoic Geological Evolution of the Foreland Basin Bordering the West Kunlun Range in Pulu Area: Constrain on Timing of Uplift of Northern Margin of the Tibet Plateau. Journal of Geophysical Research, 108(B8): 1-15. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200312002052.htm

Wang, L.Q., Pan, G.T., Li, D.M., et al., 1999. The Spatio-Temporal Framework and Geological Evolution of the Jinshajiang Arc-Basin Systems. Acta Geologica Sinica, 73(3): 206-218 (in Chinese with English abstract). http://www.researchgate.net/publication/291852423_The_Spatio-temporal_Framework_and_Geological_Evolution_of_the_Jinshajiang_Arc-Basin_Systems

Wang, X.F., Metcalfe, I., Jian, P., et al., 1999. The Stratigraphic Division and Age Determination of Jinshajiang Suture Zone. Science in China (Ser. D), 29(4): 289-297 (in Chinese).

Wang, Y.Y., Li, S.P., Wang, F.M., 2004a. Characteristics of the Basement Rock in the Xijinwulan Structure Belt and Geological Significance. Northwestern Geology, 37(1). 40-44 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_northwestern-geology_thesis/0201254329788.html

Wang, Y.Y., Wang, Y.D., Li, S.P., et al., 2004b. Characteristics of the Xijinwulan Tectonic Mélange Belt. Northwestern Geology, 37(3): 15-20 (in Chinese with English abstract).

Xi, Y.K., Wang, H.Z., 1985. Geographic Atlas of Ancient China. Map Publishing House, Beijing (in Chinese).

Yan, Q.R., Wang, Z.Q., Liu, S.W., et al., 2005. The Tethys Expansion and the Gondwana Cleavage in West-Northern Sanjiang: The SHRIMP Chronological Evidencefrom Ganzi Ophiolite Gabbro. Chinese Science Bulletin, 50(2): 158-166 (in Chinese). doi: 10.1360/csb2005-50-2-158

Yang, Z.Y., Shi, Z.J., Zhong, K.H., et al., 2010. Cun-Potential Evaluation of Multimetal Ore Resource in the Zhiduo Area, Northern Margin of the Sanjiang Metallogenetic Belt, Southern Qinghai Province. Geology and Exploration, 46(3): 426-433 (in Chinese with English abstract).

Yin, F.G., 2003. Nature and Origin of the Central Uplift in the Qiangtang Basin. Geotectonica et Metallogenia, 27(2): 143-146 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=DGYK200302005&dbcode=CJFD&year=2003&dflag=pdfdown

Yin, H.F., Zhang, K.X., 2003. PRC 1∶250 000 Donggi Conag Hu Map Regional Geological Report. China University of Geosciences Press, Wuhan, 415-416 (in Chinese).

Yong, Y.Y., Xiang, T.X., Wang, J.M., 1987. Some New Observations on North Lancangjiang Metamorphic Rocks. Contribution to the Geology of the Qinghai-Xizang (Tibet) Plateau(20), 87-89 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QZDZ199000008.htm

Zeng, S.Q., Wang, J., Chen, M., 2012. Geological Age, Paleoclimate and Petroleum Geological Characteristics of the Upper Part of the Suowa Formation in the North Qiangtang Basin. Geoscience, 26(1): 10-21(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical_xddz201201002.aspx

Zhang, K.X., He, W.H., Xu, Y.D., et al. 2014. The Sedimentary Tectonic Facies Classification and Identification Signs in China. Earth Science——Journal of China University of Geosciences, 39(8): 915-928 (in Chinese with English abstract). doi: 10.3799/dqkx.2014.086

Zhang, S.H., 2006. The Prediction of Copper, Lead-Zinc, Gold and Silver Resources Based on Comprehensive Information in the Sanjiang Area, Yunnan Province(Dissertation). Jilin University, Changchun (in Chinese with English abstract).

Zhang, S.Y., Wei, S., Wang, J.Y., et al., 1996. Magnetotelluric Sounding Research in the Qiangtang Basin, Tibet. Earth Science—Journal of China University of Geosciences, 21(2): 198-202 (in Chinese with English abstract). http://qikan.cqvip.com/Qikan/Article/Detail?id=2013196

Zhang, Z.P., 2006. A Primary Discussion in the Character of Acidolytical Hydrocarbon and Thermoluminescence Related with Gas Hydrate in Qiangtang Basin (Dissertation). China University of Geosciences, Beijing (in Chinese with English abstract).

Zhao, B., Yi, H.S., Lin, J.H., et al., 2002. Cretaceous Lithostratigraphy and Sedimentary Environment in the Ulan Ul Lake Area, Northern Qiangtang. Geological Bulletin of China, 21(11): 749-755 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200211010.htm

Zhao, X.M., Jiao, M.L., Niu, Z.J., 2006. The Recognizable Symbol of Ancient Technological in the Bayan Group Turbidite in Qumarleb Region, Qinghai. Geology and Mineral Resources of South China, (3): 48-54 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200603007.htm

Zhong, D.L., 1998. Paleo-Tethyan Orogenic Belt in West Sichuan and West Yunnan. Science Press, Beijing, 12-17 (in Chinese).

Zhong, W.L., 2012. Metallogenic Regularity of Copper Polymetallic Deposits in Zhongza-Derong in the Center of the "Jinsha-Lancang-Nu Rivers" Metallogenic Belt (Dissertation). Chengdu University of Technology, Chengdu (in Chinese with English abstract).

Zhu, C.Y., Xia, W.J., Yi, H.S., et al., 1997. The Tectonic Nature and Evolution of Mesozoic Lanping-Simao Basin. Journal of Chengdu University of Technology, 24(4): 23-30 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG704.002.htm

Zhu, Q.W., Mo, X.X., Zhang, S.Q., 1999. The Evolution of the Palaeo-Tethys in the South Lancangjiang Zone, Western Yunnan: Evidences from Magmatic Rocks. Sedimentary Geology and Tethyan Geology, 23(1): 16-30 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD199900001.htm

Zhu, Q.W., Shen, S.Y., Yang, K.H., et al., 1991. Tectono-Magmatic Types of Volcanic Rock in Lancangjiang Belt and Evolution of Tethys. Contribution to the Geology of the Qinghai-Xizang (Tibet) Plateau(21), 127-140(in Chinese with English abstract).

Zhu, Q.W., Zhang, S.Q., Tan, J., 1999. Magmatic Genesis of Volcanic Rocks of Southern Lancangjiang Convergent Margin—Magmatism about Ocean Ridge, Ocean Island and Island Arc. Geoscience, 13(2): 138-143 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ902.002.htm

Zhu, T.X., Feng, X.T., Wang, X.F., et al., 2010. Late Triassic Tectono-Palaeogeography of the Qiangtang Area on the Qinghai-Xizang Plateau. Sedimentary Geology and Tethyan Geology, 30(4): 1-10 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD201004000.htm

曾胜强, 王剑, 陈明, 等, 2012. 北羌塘盆地索瓦组上段的时代、古气候及石油地质特征. 现代地质, 26(1): 10-21. doi: 10.3969/j.issn.1000-8527.2012.01.002

陈兰, 伊海生, 时志强, 2002. 羌塘盆地雁石坪地区侏罗纪沉积物特征与沉积环境. 沉积与特提斯地质, 22(3): 80-84. doi: 10.3969/j.issn.1009-3850.2002.03.013

陈明, 罗建宁, 1999. 晚三叠世早期义敦前陆盆地的沉积特征与形成演化模式. 特提斯地质, 23(1): 108-120. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199900011.htm

陈守建, 李荣社, 计文化, 等, 2011. 巴颜喀拉构造带二叠-三叠纪岩相特征及构造演化. 地球科学——中国地质大学学报, 36(3): 393-408. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201103000.htm

戴宗明, 孙传敏, 2008. 松潘-甘孜造山带义敦岛弧中段三叠纪火山-沉积盆地的演化. 地质通报, 27(6): 799-813. doi: 10.3969/j.issn.1671-2552.2008.06.008

冯庆来, 叶玫, 章正军, 1997. 滇西早石炭世放射虫化石. 微体古生物学报, 14(1): 79-92. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT701.008.htm

付修根, 王剑, 谭富文, 2009a. 青藏高原羌塘盆地东部鄂尔陇巴组火山岩的锆石SHRIMP U-Pb年龄及其地质意义. 地质通报, 28(5): 561-567. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200905005.htm

付修根, 王剑, 吴滔, 等, 2009b. 藏北羌塘盆地大规模古风化壳的发现及其意义. 地质通报, 28(6): 696-700. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200906001.htm

苟金, 1990. 唐古拉巴音查乌马地区超基性岩的基本特征. 西北地质, (1): 1-5. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDI199001000.htm

贾建称, 吴新国, 王根厚, 等, 2006. 羌塘盆地东部中生代沉积特征与构造演化. 中国地质, 33(5): 999-1004. doi: 10.3969/j.issn.1000-3657.2006.05.007

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. 地学前缘, 10(4): 439-456. doi: 10.3321/j.issn:1005-2321.2003.04.012

简平, 汪啸风, 何龙清, 1998. 中国西南哀牢山蛇绿岩同位素地质年代学及大地构造意义. 华南地质与矿产, (1): 1-11. https://www.cnki.com.cn/Article/CJFDTOTAL-HNKC199801000.htm

寇林林, 钟康惠, 唐菊兴, 等, 2009. 昌都-思茅构造带晚三叠世构造环境的火山岩地球化学判别. 西北地质, 42(1): 79-87. doi: 10.3969/j.issn.1009-6248.2009.01.008

雷德俊, 1987. 对澜沧江以西几条主要断裂带的认识. 云南地质, 6(2): 188-196. https://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198702008.htm

李博秦, 姚建新, 高联达, 等, 2007. 西昆仑麻扎-康西瓦一带温泉沟群的形成时代及物源区分析. 地质通报, 26(4): 457-465. doi: 10.3969/j.issn.1671-2552.2007.04.012

李勇, 侯明才, 康孔, 等, 2013. 西昆仑甜水海-麻扎地块上石炭统恰提尔群B组沉积环境分析. 沉积与特提斯地质, 33(1): 55-61. doi: 10.3969/j.issn.1009-3850.2013.01.009

李勇, 王成善, 伊海生, 2002. 中生代羌塘前陆盆地充填序列及演化过程. 地层学杂志, 26(1): 62-79. doi: 10.3969/j.issn.0253-4959.2002.01.010

李勇, 王成善, 伊海生, 2003. 西藏金沙江缝合带西段晚三叠世碰撞作用与沉积响应. 沉积学报, 21(2): 191-197. doi: 10.3969/j.issn.1000-0550.2003.02.001

梁斌, 冯庆来, 王全伟, 等, 2004. 川西鲜水河断裂带拉丁期放射虫、硅质岩及构造演化意义. 中国科学(D辑), 34(7): 644-648. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200407005.htm

梁斌, 杨逢清, 郭建秋, 等, 2003. 四川雅江县上三叠统雅江组和两河口组深水遗迹化石的发现. 地质科学情报, 22(3): 41-44. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200303008.htm

米云川, 方沛英, 胡永兴, 等, 2012. 澜沧江中段昌都-普洱地块构造单元划分与演化. 云南地质, 32(4): 512-515. doi: 10.3969/j.issn.1004-1885.2012.04.024

莫宣学, 潘桂棠, 2006. 从特提斯到青藏高原形成: 构造-岩浆事件的约束. 地学前缘, 13(6): 43-51. doi: 10.3321/j.issn:1005-2321.2006.06.007

潘桂棠, 王立全, 李荣社, 等, 2012. 多岛弧盆系构造模式: 认识大陆地质的关键. 沉积与特提斯地, 32(3): 1-20. doi: 10.3969/j.issn.1009-3850.2012.03.001

潘桂棠, 王立全, 张万平, 等, 2013. 青藏高原及邻区大地构造图说明书(1∶150万). 北京: 地质出版社.

潘桂棠, 肖庆辉, 陆松年, 等, 2009. 中国大地构造单元划分. 中国地质, 36(1): 1-28. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200901004.htm

彭东, 林丽, 王全伟, 等, 2011. 甘孜-理塘结合带锰结核的发现及其地质意义. 中国地质, 38(2): 442-450. doi: 10.3969/j.issn.1000-3657.2011.02.018

彭兴阶, 罗万林, 1982. 澜沧江南段双变质带的初步确定. 青藏高原地质文集(13), 21-30. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198207004004.htm

佘宏全, 李进文, 马东方, 等, 2009. 西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP测年及地质意义. 矿床地质, 28(6): 737-746. doi: 10.3969/j.issn.0258-7106.2009.06.003

王立全, 潘桂棠, 李定谋, 等, 1999. 金沙江弧-盆系时空结构及地史演化. 地质学报, 73(3): 206-218. doi: 10.3321/j.issn:0001-5717.1999.03.002

汪啸风, Metcalfe, I., 简平, 等, 1999. 金沙江缝合带构造地层划分及时代厘定. 中国科学(D辑), 29(4): 289-297. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199904000.htm

王永文, 李善平, 王发明, 2004a. 西金乌兰构造混杂带中基底变质岩的特征和意义. 西北地质, 37(1): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDI200401007.htm

王永文, 王玉德, 李善平, 等, 2004b. 西金乌兰构造混杂岩带特征. 西北地质, 37(3): 15-20. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDI200403003.htm

奚跃昆, 王鸿祯, 1985. 中国古地理图集. 北京: 地图出版社.

闫全人, 王宗起, 刘树文, 等, 2005. 西南三江特提斯洋扩张与晚古生代东冈瓦纳裂解: 来自甘孜蛇绿岩辉长岩的SHRIMP年代学证据. 科学通报, 50(2): 158-166. doi: 10.3321/j.issn:0023-074X.2005.02.010

杨钻云, 施泽进, 钟康慧, 等, 2010. 青海南部三江成矿带北缘治多地区铁铜铅锌多金属成矿带矿产资源潜力评价. 地质与勘探, 46(3): 426-433. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201003008.htm

尹福光, 2003. 羌塘盆地中央隆起性质与成因. 大地构造与成矿学, 27(2): 143-146. doi: 10.3969/j.issn.1001-1552.2003.02.006

殷鸿福, 张克信, 2003. 中华人民共和国1: 25万东给措纳湖幅区域地质调查报告. 武汉: 中国地质大学出版社, 415-416.

雍永源, 向天秀, 王洁民, 1987. 初论北澜沧江变质岩. 青藏高原地质文集(第20集), 87-89. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199012001008.htm

张克信, 何卫红, 徐亚东, 等, 2014. 中国大陆沉积大地构造相划分与鉴别标志. 地球科学——中国地质大学学报, 39(8): 915-928.

张生辉, 2006. 云南三江地区铜铅锌金银综合信息矿产预测(学位论文). 长春: 吉林大学.

张胜业, 魏胜, 王家映, 等, 1996. 西藏羌塘盆地大地电磁测深研究. 地球科学——中国地质大学学报, 21(2): 198-202. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199602018.htm

张志攀, 2006. 羌塘盆地天然气水合物勘察的酸解烃、热释光特征初探(学位论文). 北京: 中国地质大学.

赵兵, 伊海生, 林金辉, 等, 2002. 北羌塘乌兰乌拉湖地区白垩纪岩石地层及沉积环境. 地质通报, 21(11): 749-755. doi: 10.3969/j.issn.1671-2552.2002.11.011

赵小明, 焦明路, 牛志军, 2006. 青海省曲麻莱地区巴颜喀拉山群浊积岩系识别的古遗迹学标志. 华南地质与矿产, (3): 48-54. doi: 10.3969/j.issn.1007-3701.2006.03.008

钟大赉, 1998. 川滇西部古特提斯造山带. 北京: 科学出版社, 12-17.

钟文丽, 2012. 三江成矿带中段中咱-得荣地区铜多金属矿成矿规律研究(学位论文). 成都: 成都理工大学.

朱创业, 夏文杰, 伊海生, 等, 1997. 兰坪-思茅中生代盆地性质及构造演化. 成都理工学院学报. 24(4): 23-30. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG704.002.htm

朱勤文, 莫宣学, 张双全, 1999. 南澜沧江古特提斯演化的岩浆岩证据. 特提斯地质, 23(1): 16-30. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199900001.htm

朱勤文, 沈上越, 杨开辉, 等, 1991. 澜沧江带火山岩构造-岩浆类型与特提斯演化. 青藏高原地质文集(第21集), 127-140. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199112001010.htm

朱勤文, 张双全, 谭劲, 1999. 南澜沧江结合带火山岩岩浆成因-洋脊洋岛与弧岩浆作用的性质. 现代地质, 13(2): 138-143. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ902.002.htm

朱同兴, 冯心涛, 王晓飞, 等, 2010. 青藏高原羌塘地区晚三叠世构造-古地理研究. 沉积与特提斯地质, 30(4): 1-10. doi: 10.3969/j.issn.1009-3850.2010.04.001

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(4)

Get Citation

PDF

XML

Article views (4280) PDF downloads(544)

Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic

doi: 10.3799/dqkx.2014.105

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content