Neogene Tectonic-Stratigraphic Realms and Sedimentary Sequence in China

被引：0
作者：
Song B. [1 ,2 ]
Zhang K. [1 ,2 ]
Xu Y. [2 ]
Ji J. [2 ]
Luo M. [2 ]
Han F. [3 ]
Hou Y. [1 ]
Ai K. [4 ]
机构：
[1] Institute of Geological Survey, China University of Geosciences, Wuhan
[2] State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan
[3] School of Earth Sciences, East China University of Technology, Nanchang
[4] School of Resource and Environmental Engineering, Mianyang Teachers' College, Mianyang
来源：
Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences | 2022年 / 47卷 / 04期
关键词：
Neogene; Sedimentary basin; Stratigraphic correlation; Stratigraphy; Tectonic-stratigraphic division;
D O I：
10.3799/dqkx.2021.072
中图分类号：
学科分类号：
摘要：
Neogene is the key period for the establishment of geomorphology and pattern of climate changes in China, involving the significant uplift of Tibetan Plateau and final formation of modern plateau landform, the termination of seafloor spreading for the South China Sea, the final establishment of the present large river system in East Asia, the final establishment of the west-tilting topography of China, the formation and enhancement of East Asian monsoon system. Through the comprehensive study of Neogene tectonics, sedimentary basins (groups), volcanic rocks, uplifting belts and large deformation structures in China, 10 first-order tectonic-stratigraphic units (super-realms) and 27 second-order tectonic-stratigraphic units (realms) have been subdivided, including 94 basins. Through the research of the types of basins in each unit, sedimentary sequence, sedimentary age and stratigraphic contact, the Neogene lithostratigraphic correlation framework in China was established and the sedimentary-tectonic-climate history was summarized. © 2022, Editorial Department of Earth Science. All right reserved.
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页码：1143 / 1161
页数：18
相关论文
共 154 条
[1]  
Ai K.K., Shi G.L., Zhang K.X., Et al., The Uppermost Oligocene Kailas Flora from Southern Tibetan Plateau and Its Implications for the Uplift History of the Southern Lhasa Terrane, Palaeogeography, Palaeoclimatology, Palaeoecology, 515, pp. 143-151, (2019)
[2]  
Aitchison J.C., Davis A.M., Badengzhu, Et al., New Constraints on the India-Asia Collision: The Lower Miocene Gangrinboche Conglomerates, Yarlung Tsangpo Suture Zone, SE Tibet, Journal of Asian Earth Sciences, 21, 3, pp. 251-263, (2002)
[3]  
An Z.S., Late Cenozoic Climate Change in Asia: Loess, Monsoon and Monsoon-Arid Environment Evolution, (2014)
[4]  
An Z.S., Kutzbach J.E., Prell W.L., Et al., Evolution of Asian Monsoons and Phased Uplift of the Himalaya-Tibetan Plateau since Late Miocene Times, Nature, 411, 6833, pp. 62-66, (2001)
[5]  
Briais A., Patriat P., Tapponnier P., Updated Interpretation of Magnetic Anomalies and Seafloor Spreading Stages in the South China Sea: Implications for the Tertiary Tectonics of Southeast Asia, Journal of Geophysical Research: Solid Earth, 98, B4, pp. 6299-6328, (1993)
[6]  
Stratigraphy (Lithostratic) of Yunnan Province, (1996)
[7]  
Cao K., Mai H.T., Wang G.C., Et al., Mesozoic-Cenozoic Tectonic and Topographic Development of the Pamir Syntaxis and Its Potential Effects on the Sea Retreat in the Tarim Basin, Quaternary Science, 38, 1, pp. 15-38, (2018)
[8]  
Cao K., Xu Y.D., Wang G.C., Et al., Neogene Source-to-Sink Relations between the Pamir and Tarim Basin: Insights from Stratigraphy, Detrital Zircon Geochronology, and Whole-Rock Geochemistry, The Journal of Geology, 122, 4, pp. 433-454, (2014)
[9]  
Chen F.N., Xu Y.D., Jiang S.S., Et al., Late Miocene-Early Pleistocene Ostracoda Fauna of Oma Formation in Gyirong Basin, Southern Tibet, Earth Science, 35, 5, pp. 821-827, (2010)
[10]  
Chen H.H., Han J.T., Ding Z.L., Et al., The Sedimentary Sequence Era of Wuyu Basin in the Southern Tibet since the Late Cenozoic and Its Tectonic Significance, Science in China (Series D), 37, 12, pp. 1617-1624, (2007)
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