维西地区中三叠统上兰组物源分析及构造背景判断

王启宇; 牟传龙; 贺娟; 闫国川; 凌亚军; 孙小勇

doi:10.3799/dqkx.2018.307

Volume 43 Issue 8

Aug. 2018

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Article Navigation > Earth Science > 2018 > 43(8): 2811-2832

Wang Qiyu, Mou Chuanlong, He Juan, Yan Guochuan, Ling Yajun, Sun Xiaoyong, 2018. Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area. Earth Science, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307

Citation:

Wang Qiyu, Mou Chuanlong, He Juan, Yan Guochuan, Ling Yajun, Sun Xiaoyong, 2018. Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area. Earth Science, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307

Citation:

Wang Qiyu, Mou Chuanlong, He Juan, Yan Guochuan, Ling Yajun, Sun Xiaoyong, 2018. Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area. Earth Science, 43(8): 2811-2832. doi: 10.3799/dqkx.2018.307

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Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area

doi: 10.3799/dqkx.2018.307

Wang Qiyu^{1,2
,},
Mou Chuanlong^{1,2
,
,},
He Juan²,
Yan Guochuan³,
Ling Yajun⁴,
Sun Xiaoyong⁵

1.
College of Earth Sciences and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
2.
Chengdu Center of China Geological Survey, Chengdu 610081, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
4.
No. 106 Geological Brigade of Sichuan Bureau of Geology and Mineral Resources, Chengdu 611130, China
5.
Northwest Sichuan Geological Brigade of Sichuan Bureau of Geology and Mineral Resources, Mianyang 621000, China

Received Date: 2018-04-05
Publish Date: 2018-08-15

Abstract

Abstract

There was little research on the formation and evolution of the Triassic clastic rocks in the Jinshajiang tectonic belt, undermining the overall understanding of the evolution history of the Jinshajiang ocean basin.It is found in this study the protolithes of Shanglan Formation are mainly sandstone and shale, which is in agreement with the classification discriminate diagram of clastic rocks.The U-Pb dating of detrital zircon show 4 age groups, which are 426-603 Ma, 713-980 Ma, 1 000-1 600 Ma and 1 600-2 500 Ma respectively, indicative of the provenance from basement of the Yangtze block and its vincinity, magmatism of homochronous Pan-African and Caledonian.The content of ∑REE are slightly higher compared with that of upper crust.The LREE and HREE show obvious fractionation, (La/Yb)_N=5.23-12.33.Meanwhile, δEu is slightly abnormal.The characteristics of detrital component and discrimination diagram show the provenance are mainly from collisional orogenic belt and a little from volcanic arcs.The quality of the matters belong to old sediment and quartz-feldspathic volcanic.The tectonic setting of provenance in Shanglan Formation is mainly continental arc and active continental margin.The information above common indicates that the tectonic setting of Shanglan Formation is depression which was formed by extruding of subduction collision.Combined with regional tectonic evolution, we consider its tectonic environment was retroarc foreland basin.
- zircon U-Pb age,
- provenance,
- tectonic setting,
- Shanglan Formation,
- Weixi area,
- geochemistry,
- geochronology

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References(86)

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Provenance Analysis and Tectonic Setting Judgment in Shanglan Formation of Middle Triassic in Weixi Area

doi: 10.3799/dqkx.2018.307

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