渭河-三门峡盆地三门组沉积充填特征、物源区及其构造意义

刘瑾; 陈兴强; 王平; 李廷栋

doi:10.3799/dqkx.2020.112

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2673-2683

Liu Jin, Chen Xingqiang, Wang Ping, Li Tingdong, 2020. Sedimentary Characteristics, Provenance and Tectonic Significance of the Sanmen Formation in Weihe-Sanmenxia Basin. Earth Science, 45(7): 2673-2683. doi: 10.3799/dqkx.2020.112

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Liu Jin, Chen Xingqiang, Wang Ping, Li Tingdong, 2020. Sedimentary Characteristics, Provenance and Tectonic Significance of the Sanmen Formation in Weihe-Sanmenxia Basin. Earth Science, 45(7): 2673-2683. doi: 10.3799/dqkx.2020.112

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Sedimentary Characteristics, Provenance and Tectonic Significance of the Sanmen Formation in Weihe-Sanmenxia Basin

doi: 10.3799/dqkx.2020.112

1.
School of Civil and Architecture Engineering, Xi'an Technological University, Xi'an 710021, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
China Railway First Survey and Design Institute Group Co., Ltd., Xi'an 710043, China
4.
School of Geography, Nanjing Normal University, Nanjing 210023, China

Received Date: 2020-05-12
Publish Date: 2020-07-15

Abstract

Abstract

Sanmen Formation, deposited in Weihe basin and Sanmenxia basin, recorded the regional sedimentary history from Pliocene to Pleistocene. This formation is of great significance to understand regional paleoenvironment and basin evolution. The sedimentary facies analysis and source reconstruction of Sanmen Formation indicated a great environment changes in 2.8-2.6 Ma, Weihe basin changed from deep lake to shallow lake deposition in 2.8-2.6 Ma, with the water level decreasing, while Sanmenxia basin changed from fluvial facies to shore-shallow lake, with the water level rising. Combined with the results of paleogeomorphic reconstruction and regional stress inversion, Weihe basin and Sanmenxia basin were properbably independent with each other in Pliocene. In the Early Pleistocene, these two basins were connected. The water in Weihe basin flow into Sanmenxia basin, forming the Paleo-Sanmen Lake. By comparing the results of regional tectonic events and provenance analysis, it is concluded that the rapid uplift of Tibet Plateau may be the trigger force of the basin and regional drainage evolution.
- Weihe basin,
- Sanmenxia basin,
- Sanmen Formation,
- neotectonics,
- tectonics

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References(65)

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Sedimentary Characteristics, Provenance and Tectonic Significance of the Sanmen Formation in Weihe-Sanmenxia Basin

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