青藏高原古近纪—新近纪隆升与沉积盆地分布耦合

张克信; 王国灿; 陈奋宁; 徐亚东; 骆满生; 向树元; 寇晓虎; 赵来时

Volume 32 Issue 5

Sep. 2007

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Article Navigation > Earth Science > 2007 > 32(5): 583-597

ZHANG Ke-xin, WANG Guo-can, CHEN Fen-ning, XU Ya-dong, LUO Man-sheng, XIANG Shu-yuan, KOU Xiao-hu, ZHAO Lai-shi, 2007. Coupling between the Uplift of Qinghai-Tibet Plateau and Distribution of Basins of Paleogene-Neogene. Earth Science, 32(5): 583-597.

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Coupling between the Uplift of Qinghai-Tibet Plateau and Distribution of Basins of Paleogene-Neogene

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Environmental Geology, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2007-06-16
Publish Date: 2007-09-25

Abstract

Abstract

Recent effort on comprehensive geological mapping in the Qinghai-Tibet plateau and adjacent regions permits recognition of 92 remnant sedimentary basins filled with the Paleogene-Neogene sediments. The relatively large basins with complete Paleogene-Neogene sequences are seen around the margins and at central part of the plateau. Most of the slip-pull basins are distributed along the major faults in the southern, northern, and eastern margins of the plateau. The marine Paleogene-Neogene successions are limited to the southern Tibet and the Yecheng area of Xinjiang. Both the subabyssal and abyssal sequences are exposed at the Gyangze, Saga, Guoyala and Sangmai areas. The deep-water facies successions outcrop in the west, while the shallow-water facies sequences in the east, indicating the closure of the Neo-Tethys Ocean occurring earlier in the east and then in the west. Tectonic uplift of the Qinghai-Tibet plateau occurred first in its eastern part. During the Late Cretaceous, tectonic uplift of the Plateau occurred in its northeastern part and configuration of the Plateau was characterized by paleo-highs in the northeast and depressions in the west. In Paleocene-Eocene interval, the Tengchun-Bange and Kuyake-Golmud areas experienced local tectonic uplifting; the West Kunlun uplift zone broadened easterly; the Qilian uplift zone broadened southerly; the Sunpa-Ganzi uplift zone shrank easterly. The Oligocene configuration of the Plateau was characterized by mountain chains rising along its margins and sedimentary basins occurring in the central part because of tectonic uplifts of the Gangdise and Himalaya blocks. In the same time, the Kunlun-Arjin-Qilian uplift zones have broadened southerly and northerly. In contrast, the expended uplift zones of the Gangdise, Himalaya, Karakorum, and Kunlun blocks feature the paleogeographic contours of the Qinghai-Tibet Plateau during the Miocene-Pliocene. As a result, the paleogeographic configurations of the Qinghai-Tibet Plateau turned over during the Cretaceous-Pliocene transition, with high contours in the east in the pre-Oligocene switching to the high contours in the west at the end-Pliocene. The uplift of the Qinghai-Tibet Plateau during Cenozoic is episodic and the uplifts of various blocks within the Plateau are different in space and time.
- Paleogene-Neogene,
- sediment basin,
- stratigraphic sequence,
- the paleogeographic configurations,
- Qinghai-Tibet Plateau,

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Coupling between the Uplift of Qinghai-Tibet Plateau and Distribution of Basins of Paleogene-Neogene

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