西藏聂荣微陆块奥陶纪和侏罗纪岩浆事件的年龄证据

陆露; 钱程; 赵珍; 吴珍汉; 刘玉双; 周亮; 王岩

doi:10.3799/dqkx.2018.712

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1110-1124

Lu Lu, Qian Cheng, Zhao Zhen, Wu Zhenhan, Liu Yushuang, Zhou Liang, Wang Yan, 2018. Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet. Earth Science, 43(4): 1110-1124. doi: 10.3799/dqkx.2018.712

Citation:

Lu Lu, Qian Cheng, Zhao Zhen, Wu Zhenhan, Liu Yushuang, Zhou Liang, Wang Yan, 2018. Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet. Earth Science, 43(4): 1110-1124. doi: 10.3799/dqkx.2018.712

Citation:

Lu Lu, Qian Cheng, Zhao Zhen, Wu Zhenhan, Liu Yushuang, Zhou Liang, Wang Yan, 2018. Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet. Earth Science, 43(4): 1110-1124. doi: 10.3799/dqkx.2018.712

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Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet

doi: 10.3799/dqkx.2018.712

Lu Lu^{1,2
,},
Qian Cheng³,
Zhao Zhen⁴,
Wu Zhenhan⁴,
Liu Yushuang^1,2,
Zhou Liang⁵,
Wang Yan¹

1.
Paleontological College, Shenyang Normal University, Shenyang 110034, China
2.
Key Laboratory of Evolution of Past Life in Northeast Asia, Ministry of Land and Resources, Shenyang 110034, China
3.
Shenyang Institute of Geology and Mineral Resources, Shenyang 110000, China
4.
Chinese Academy of Geological Sciences, Beijing 100081, China
5.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

In order to deepen our knowledge and understanding about the tectonic evolution of the Bangonghu-Nujiang suture zone(BNS), zircon U-Pb dating was conducted for granitic gneiss and granodioritic gneiss of Nyainrong microcontinent by LA-ICP-MS in this study. Results show two groups of average zircon U-Pb ages, with one of 453.7±2.5 Ma, and the other of 176.6±1.1 Ma and 178.04±0.8 Ma. ⁴⁰Ar-³⁹Ar dating was conducted for biotite from granitic gneiss and muscovite from granodioritic gneiss in Nyainrong microcontinent.The ⁴⁰Ar-³⁹Ar plateau ages yield 161.8±1.1 Ma and 178.9±1.2 Ma, respectively, showing that the study area experienced the Late Ordovician and the Early Jurassic magmatic events. Combined with field condition and study results, it is suggested that the Ordovician magmatic event was related to the Early Paleozoic orogeny which could be caused by proto-Tethyan oceanic subduction along Gondwana continental margin, and the Jurassic magmatic event was related to the subduction and closure of the Bangong-Nujiang oceanic crust.
- Tibetan plateau,
- Nyainrong microcontinent,
- zircon U-Pb age,
- ⁴⁰Ar-³⁹Ar age,
- Bangonghu-Nujiang suture zone,
- geochronology

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References(96)

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Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet

doi: 10.3799/dqkx.2018.712

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