青藏高原中-南部新生代构造演化的热年代学制约

朱晓青; 郭兴伟; 张训华; 侯方辉; 温珍河; 耿威; 王忠蕾; 孙建伟; 祁江豪

doi:10.3799/dqkx.2018.532

Volume 43 Issue 6

Jun. 2018

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Zhu Xiaoqing, Guo Xingwei, Zhang Xunhua, Hou Fanghui, Wen Zhenhe, Geng Wei, Wang Zhonglei, Sun Jianwei, Qi Jianghao, 2018. Thermochronological Constraints on Cenozoic Tectonic Evolution of South-Central Qinghai-Tibet Plateau. Earth Science, 43(6): 1903-1920. doi: 10.3799/dqkx.2018.532

Citation:

Zhu Xiaoqing, Guo Xingwei, Zhang Xunhua, Hou Fanghui, Wen Zhenhe, Geng Wei, Wang Zhonglei, Sun Jianwei, Qi Jianghao, 2018. Thermochronological Constraints on Cenozoic Tectonic Evolution of South-Central Qinghai-Tibet Plateau. Earth Science, 43(6): 1903-1920. doi: 10.3799/dqkx.2018.532

Citation:

Zhu Xiaoqing, Guo Xingwei, Zhang Xunhua, Hou Fanghui, Wen Zhenhe, Geng Wei, Wang Zhonglei, Sun Jianwei, Qi Jianghao, 2018. Thermochronological Constraints on Cenozoic Tectonic Evolution of South-Central Qinghai-Tibet Plateau. Earth Science, 43(6): 1903-1920. doi: 10.3799/dqkx.2018.532

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Thermochronological Constraints on Cenozoic Tectonic Evolution of South-Central Qinghai-Tibet Plateau

doi: 10.3799/dqkx.2018.532

Zhu Xiaoqing^{1,2
,},
Guo Xingwei^{1,2
,
,},
Zhang Xunhua^2,3,
Hou Fanghui^1,2,
Wen Zhenhe^1,2,
Geng Wei^1,2,
Wang Zhonglei^1,2,
Sun Jianwei^1,2,
Qi Jianghao^1,2

1.
Qingdao Institute of Marine Geology, Qingdao 266071, China
2.
Laboratory for Marine Mineral Resources, National Laboratory for Marine Science and Technology, Qingdao 266237, China
3.
Nanjing Center, China Geological Survey, Nanjing 210016, China

Received Date: 2017-12-06
Publish Date: 2018-06-15

Abstract

Abstract

The spatial and temporal characteristics of the uplift in the Qinghai-Tibet Plateau since the Cenozoic has long been debated. Medium-and low-temperature thermochronological analysis on the base rocks plays an important role in detecting the uplifting processes of the plateau. Here we collected 15 intermediate-acid and metamorphic rock samples distributed in the Tibetan Plateau. Zircon and apatite fission track (ZFT and AFT) analyses were performed on these samples in order to provide constraints on the uplifting process of the plateau since the Mesozoic. 10 samples' ZFT results show that the ZFT ages range from 182 Ma to 33 Ma, probably recording collisions among different terranes or tectonothermal events in the Tibetan plateau before the Oligocene. Specially, ZFT ages of 3 samples distributed around the Yarlung Zangbo suture zone range from Late Eocene to Early Oligocene, which implies that a hard continent-continent collision occurred during ca. 36 to ca. 33 Ma. The Neocene ages dominate the AFT results, varying from 70.4 Ma to 5.0 Ma. Combined with the AFT reversed modeling results, it is concluded that southern part of Qinghai-Tibet Plateau has apparently experienced uplift since the Middle-Late Miocene. The uplift rates increased rapidly after ca. 5 Ma to ca. 4 Ma. The AFT ages become younger towards southeastern part of the Qinghai-Tibetan Plateau, implying the India and Asia continent collision controls the uplifting process of the Tibetan Plateau. Additionally, the central part of the plateau might have reached high altitude in the Late Cretaceous-Eocene and have kept very low denudation rate up to now.
- Tibet Plateau,
- thermochronology,
- thermal reversed modeling,
- Cenozoic,
- hard collision,
- structural geology

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References(108)

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Thermochronological Constraints on Cenozoic Tectonic Evolution of South-Central Qinghai-Tibet Plateau

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