南秦岭北缘淅川地区泥盆纪地层的物源及构造背景

徐大良; 彭练红; 刘浩; 邓新; 魏运许; 张维峰

doi:10.3799/dqkx.2018.591

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2234-2248

Xu Daliang, Peng Lianhong, Liu Hao, Deng Xin, Wei Yunxu, Zhang Weifeng, 2018. Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block. Earth Science, 43(7): 2234-2248. doi: 10.3799/dqkx.2018.591

Citation:

Xu Daliang, Peng Lianhong, Liu Hao, Deng Xin, Wei Yunxu, Zhang Weifeng, 2018. Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block. Earth Science, 43(7): 2234-2248. doi: 10.3799/dqkx.2018.591

Citation:

Xu Daliang, Peng Lianhong, Liu Hao, Deng Xin, Wei Yunxu, Zhang Weifeng, 2018. Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block. Earth Science, 43(7): 2234-2248. doi: 10.3799/dqkx.2018.591

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Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block

doi: 10.3799/dqkx.2018.591

Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2017-10-31
Publish Date: 2018-07-15

Abstract

Abstract

The Devonian sedimentary strata, widely developed in the Qinling orogenic belt, are good vehicles to reveal the ocean-continent transition, tectonic attributes and tectonic settings of the Qinling orogenic belt in the Middle Paleozoic. This study presents new geochemical and zircon U-Pb isotopic data for the Devonian sedimentary rocks in Xichuan area. Geochemical data show that the Devonian clastic rocks are characterized by moderate compositional maturity, and a higher portion of sediment recycling, and are likely to have been derived predominantly from felsic igneous rocks within upper-continental-crust. The detrital zircon ages are mainly concentrated in Late Neoproterozoic-Paleozoic (0.40-0.63 Ga), Neoproterozoic (0.7-0.9 Ga) and Mesoproterozoic (1.0-1.6 Ga), with a small amount of ages in Paleoproterozoic and Middle-Late Archean. Comprehensive analysis suggests that the Devonian basin in Xichuan area has beea formed in passive continental margin, and its provenance may be mainly the uplift basement and tectonic highland of the South Qinling, not from the North Qinling. The subduction accretion event along the Shangdan Ocean probably did not affect the interior of South Qinling.
- South Qingling,
- detrital zircon geochronology,
- Devonian,
- provenance analysis,
- tectonic affinity,
- geochemistry

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Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block

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