拉萨地块北缘中晚侏罗世周缘前陆盆地的厘定

李奋其; 张士贞; 李俊; 刘函; 秦雅东

doi:10.3799/dqkx.2021.047

Volume 47 Issue 2

Feb. 2022

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Article Navigation > Earth Science > 2022 > 47(2): 387-404

Li Fenqi, Zhang Shizhen, Li Jun, Liu Han, Qin Yadong, 2022. Definition of Mid-Late Jurassic Peripheral Foreland Basin in the Northern Margin of Lhasa Block. Earth Science, 47(2): 387-404. doi: 10.3799/dqkx.2021.047

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Li Fenqi, Zhang Shizhen, Li Jun, Liu Han, Qin Yadong, 2022. Definition of Mid-Late Jurassic Peripheral Foreland Basin in the Northern Margin of Lhasa Block. Earth Science, 47(2): 387-404. doi: 10.3799/dqkx.2021.047

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Definition of Mid-Late Jurassic Peripheral Foreland Basin in the Northern Margin of Lhasa Block

doi: 10.3799/dqkx.2021.047

Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2021-04-22
Publish Date: 2022-02-25

Abstract

Abstract

To identify its types and evolution features of the Mid-Late Jurassic basin located in northern margin of Lhasa block is of great significance for reconstructing its tectonic-paleogeography and assessing the petroliferous basins in Bangonghu-Nujiang junction zone and its adjacent area. In this paper, the sedimetary features and provenance area of Mid-Late Jurassic Lagongtang Fm which is exposed in north of Nagqu county, was studied. The results shows that the Member 1 of Lagongtang Fm belongs to steep-slope delta deposition, and debris flow deposits located in its lower part has the characterisitics of southward flow, and Member 2 of the Fm was deposted in tidal flats and mixed shelf, and the detrital zircon ages of greywackes in the lower part of Member 1 and quartz fine sandstone in the lower part of Member 2 range from 2 611 Ma to 216 Ma and from 2 800 Ma to 152 Ma respectively. Comprehensive research results shows that the basin located in northern marigin of Lhasa block is a peripheral foreland one controlled by Bangonghu-Nujiang junction zone, and had dual source supply, and experienced the conversion from flysch basin to molasses one at 152 Ma or so. Meanwhile, the overthrust which took place in Bangonghu-Nujiang junction zone become stronger than before since that time, and caused a new foreland basin marked by the Shamuluo Formation form in it.
- Lagongtang Formation,
- Bangonghu-Nujiang junction zone,
- peripheral foreland basin,
- provenance area,
- Mid-Late Jurassic,
- Shamuluo Formation,
- tectonics

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Definition of Mid-Late Jurassic Peripheral Foreland Basin in the Northern Margin of Lhasa Block

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