川西若尔盖地区中-新生代构造-热事件及其年代学框架

邓宾; 刘树根; 刘顺; 李祥辉; 李巨初; 李智武

doi:10.3799/dqkx.2013.031

Volume 38 Issue 2

Mar. 2013

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Article Navigation > Earth Science > 2013 > 38(2): 317-328

DENG Bin, LIU Shu-gen, LIU Shun, LI Xiang-hui, LI Ju-chu, LI Zhi-wu, 2013. Tectono-Thermal Events and Chronological Framework in Zoige and Its Periphery. Earth Science, 38(2): 317-328. doi: 10.3799/dqkx.2013.031

Citation:

DENG Bin, LIU Shu-gen, LIU Shun, LI Xiang-hui, LI Ju-chu, LI Zhi-wu, 2013. Tectono-Thermal Events and Chronological Framework in Zoige and Its Periphery. Earth Science, 38(2): 317-328. doi: 10.3799/dqkx.2013.031

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Tectono-Thermal Events and Chronological Framework in Zoige and Its Periphery

doi: 10.3799/dqkx.2013.031

1.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China
2.
School of Earth Sciences and Engineering Nanjing University, Nanjing 210093, China

Received Date: 2012-04-15
Publish Date: 2013-03-01

Abstract

Abstract

Based on analysis of the sedimentary features, fission track data, ESR dating and Ar-Ar dating, we argue that there are seven tectono-thermal events in Zoige and its periphery from the Late Triassic. The first tectono-thermal events (D₁) took place at the end of the Carnian to the beginning of the Norian stage to form the tectonic framework of Zoige area; the second (D₂) and the fourth (D₄) tectono-thermal events took place at the early of Jurassic (200－180 Ma) and 130-110 Ma, respectively. They are the key change events in tectonic framework at each time. The seventh (D₇) took place at the early of Miocene (~20 Ma), as the most important tectonic event to form the Tibet Plateau. The other three events (D₃, D₅, D₆) took place at 160－140 Ma, 70－60 Ma, 50－40 Ma, respectively.
- aptatite fission track,
- ESR dating,
- geochronology,
- tectono-thermal events,
- Zoige,
- eastern margin of Tibet

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References(83)

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Tectono-Thermal Events and Chronological Framework in Zoige and Its Periphery

doi: 10.3799/dqkx.2013.031

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