昌宁-孟连结合带中三叠世含放射虫硅质岩地层的古特提斯意义

罗亮; 谢韬; 王冬兵; 黄晓明; 姜丽莉; 李建忠; 彭智敏

doi:10.3799/dqkx.2020.093

Volume 45 Issue 8

Aug. 2020

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Article Navigation > Earth Science > 2020 > 45(8): 3014-3027

Luo Liang, Xie Tao, Wang Dongbing, Huang Xiaoming, Jiang Lili, Li Jianzhong, Peng Zhimin, 2020. Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys. Earth Science, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093

Citation:

Luo Liang, Xie Tao, Wang Dongbing, Huang Xiaoming, Jiang Lili, Li Jianzhong, Peng Zhimin, 2020. Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys. Earth Science, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093

Citation:

Luo Liang, Xie Tao, Wang Dongbing, Huang Xiaoming, Jiang Lili, Li Jianzhong, Peng Zhimin, 2020. Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys. Earth Science, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093

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Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys

doi: 10.3799/dqkx.2020.093

Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2020-02-19
Publish Date: 2020-08-15

Abstract

Abstract

The Middle Triassic strata in the Changning-Menglian suture zone record the evolution of the Paleo-Tethys Ocean in the late stage, providing an important window for the better understanding of the structure and geography of the Paleo-Tethys. The original Devonian Manxin Formation composed of siliceous, mudstone and sandstone interlayer (lens bodies) in Tuanjie area, Cangyuan County, Yunnan Province. The zircon U-Pb dating of arkose and geochemical analysis of siliceous rocks were carried out, respectively, and the significance of the Paleo-Tethys evolution was explored on the basis of limiting the formation age. Zircon U-Pb dating of arkose lens bodies and interlayers shows that their ages are not earlier than 237.8±1.3 Ma and 237.7±1.4 Ma, respectively, the stratum can be compared with the Muyinhe Formation. The discovery of the Middle Triassic stratum fills the blank of the sedimentary records in this area. Geochemical analysis of the siliceous rock in this stratum indicates that it was formed in the continental marginal environment. Combining with composition of granule in sedimentary rock and para-mineral characteristics, it shows that the scale of the residual oceanic basin of Paleo-Tethys is limited. The angular inconsistency of the molassic-type deposition of the Sanchahe Formation above the early stratum indicates the final closure of the residual ocean basin.
- zircon U-Pb dating,
- geochemistry,
- radiolarian chert,
- Muyinhe Formation,
- residual basin,
- geochronology

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References(99)

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Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys

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