湘东南中泥盆统石英砂砾岩物源分析及其大地构造意义

陈家驹; 徐先兵; 梁承华; 徐亚东

doi:10.3799/dqkx.2021.022

Volume 46 Issue 10

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(10): 3421-3434

Chen Jiaju, Xu Xianbing, Liang Chenghua, Xu Yadong, 2021. Provenance Analysis and Tectonic Implications of Middle Devonian Quartzose Conglomerate and Sandstone in Southeastern Hunan Province, South China. Earth Science, 46(10): 3421-3434. doi: 10.3799/dqkx.2021.022

Citation:

Chen Jiaju, Xu Xianbing, Liang Chenghua, Xu Yadong, 2021. Provenance Analysis and Tectonic Implications of Middle Devonian Quartzose Conglomerate and Sandstone in Southeastern Hunan Province, South China. Earth Science, 46(10): 3421-3434. doi: 10.3799/dqkx.2021.022

Citation:

Chen Jiaju, Xu Xianbing, Liang Chenghua, Xu Yadong, 2021. Provenance Analysis and Tectonic Implications of Middle Devonian Quartzose Conglomerate and Sandstone in Southeastern Hunan Province, South China. Earth Science, 46(10): 3421-3434. doi: 10.3799/dqkx.2021.022

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Provenance Analysis and Tectonic Implications of Middle Devonian Quartzose Conglomerate and Sandstone in Southeastern Hunan Province, South China

doi: 10.3799/dqkx.2021.022

School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-02-01
Available Online: 2021-11-03
Publish Date: 2021-11-03

Abstract

Abstract

The formation and denudation of the Early Paleozoic Jiangnan uplift can be used to restrict the Kwangsian orogeny and its dynamic mechanism in South China. Based on detrital zircon U-Pb geochronology and trace element geochemistry of the quartzose conglomerate of the Middle Devonian Tiaomajian Formation in Nanwan, south of the Jiangnan Uplift, the provenance and tectonic significance of the conglomerate are discussed. U-Pb ages of 270 available detrital zircons from the four samples consist of main peaks of 430-440 Ma and sub-peaks of 800-1 100 Ma, 1 700-2 000 Ma and 2 400-2 600 Ma. Zircon CL images, Th/U ratios and REE partition patterns indicate that detrital zircons are dominated by magmatic zircons, with only a small amount of metamorphic and hydrothermal zircons. The mineral morphology, composition and maturity indicate that the source area is near source and deposited in coastal environment. The comprehensive source analysis shows that the provenance of the quartzite conglomerate of the Middle Devonian Tiaomajian Formation in southeastern Hunan is from the Jiangnan Uplift on the north side. The Jiangnan uplift was formed during the Kwangsian period of intracontinental orogeny. The trace element geochemical characteristics of the Early Paleozoic magmatic zircons indicate that they are of continental type and formed in a continental arc tectonic setting. Combined with the regional geological characteristics, the Kwangsian orogeny in South China is the product of oceanic subduction on its southern side, which is related to the aggregation of Gondwana continent.
- Middle Devonian Tiaomajian Formation,
- detrital zircon U-Pb age,
- provenance analysis,
- Jiangnan uplift,
- Kwangsian orogeny in South China block,
- sedimentology

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References(88)

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Provenance Analysis and Tectonic Implications of Middle Devonian Quartzose Conglomerate and Sandstone in Southeastern Hunan Province, South China

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