冈底斯中部松多岩组形成时代及物源:来自碎屑锆石U-Pb年代学证据

解超明; 宋宇航; 王明; 范建军; 张红雨; 郝宇杰

doi:10.3799/dqkx.2019.024

Volume 44 Issue 7

Jul. 2019

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Xie Chaoming, Song Yuhang, Wang Ming, Fan Jianjun, Zhang Hongyu, Hao Yujie, 2019. Age and Provenance of Sumdo Formation in Central Gangdise, Tibetan Plateau: Detrital Zircon U-Pb Geochronological Evidence. Earth Science, 44(7): 2224-2233. doi: 10.3799/dqkx.2019.024

Citation:

Xie Chaoming, Song Yuhang, Wang Ming, Fan Jianjun, Zhang Hongyu, Hao Yujie, 2019. Age and Provenance of Sumdo Formation in Central Gangdise, Tibetan Plateau: Detrital Zircon U-Pb Geochronological Evidence. Earth Science, 44(7): 2224-2233. doi: 10.3799/dqkx.2019.024

Citation:

Xie Chaoming, Song Yuhang, Wang Ming, Fan Jianjun, Zhang Hongyu, Hao Yujie, 2019. Age and Provenance of Sumdo Formation in Central Gangdise, Tibetan Plateau: Detrital Zircon U-Pb Geochronological Evidence. Earth Science, 44(7): 2224-2233. doi: 10.3799/dqkx.2019.024

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Age and Provenance of Sumdo Formation in Central Gangdise, Tibetan Plateau: Detrital Zircon U-Pb Geochronological Evidence

doi: 10.3799/dqkx.2019.024

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China

Received Date: 2018-11-18
Publish Date: 2019-07-15

Abstract

Abstract

The Sumdo Formation, which is widely developed in the central Gangdise, has been controversial in its stratigraphic age due to lack of fossil evidence, seriously restricting our understanding of structural evolution in the Sumdo area. In this paper, on the basis of detailed field geological investigation, LA-ICP-MS U-Pb dating was carried out on detrital zircons from metamorphic sandstones of Sumdo Formation. The minimum zircon age of detrital zircon in metamorphic sandstones is 316 Ma, the Late Carboniferous, representing the lower limit of the main depositional age of the Sumdo Formation. Provenance analysis indicates that the sedimentary detritus was sourced from the Lhasa terrane itself (South and North Lhasa terranes), and may be the sedimentary record of the initial ocean basin of Sumdo Paleo-Tethys Ocean. The determination of the age of the Sumdo Formation has further improved the Late Paleozoic stratigraphic system in this area and is of great significance to the study of lithofacies and paleogeography of the Late Carboniferous-Early Permian in the northern margin of the Gondwana.
- Tibetan Plateau,
- Gangdise,
- Late Carboniferous-Early Permian,
- Sumdo Formation,
- detrital zircon,
- provenance,
- geochronology

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References(56)

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