华南板块东南部南华纪‒震旦纪沉积地层区域对比、物源特征及构造演化

宋芳; 何垚砚; 牛志军; 杨文强; 王志宏

doi:10.3799/dqkx.2023.158

Volume 49 Issue 9

Sep. 2024

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Article Navigation > Earth Science > 2024 > 49(9): 3411-3427

Song Fang, He Yaoyan, Niu Zhijun, Yang Wenqiang, Wang Zhihong, 2024. Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block: Implications for Tectonic Evolution. Earth Science, 49(9): 3411-3427. doi: 10.3799/dqkx.2023.158

Citation:

Song Fang, He Yaoyan, Niu Zhijun, Yang Wenqiang, Wang Zhihong, 2024. Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block: Implications for Tectonic Evolution. Earth Science, 49(9): 3411-3427. doi: 10.3799/dqkx.2023.158

Citation:

Song Fang, He Yaoyan, Niu Zhijun, Yang Wenqiang, Wang Zhihong, 2024. Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block: Implications for Tectonic Evolution. Earth Science, 49(9): 3411-3427. doi: 10.3799/dqkx.2023.158

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Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block: Implications for Tectonic Evolution

doi: 10.3799/dqkx.2023.158

Song Fang^{1, 2
,
,},
He Yaoyan^{1, 2},
Niu Zhijun^{1, 2},
Yang Wenqiang^{1, 2},
Wang Zhihong^{1, 2}

1.
Hubei Key Laboratory of Paleontology and Geological Environment Evolution, Wuhan 430205, China
2.
Wuhan Center, China Geological Survey (Geosciences Innovation Center of Central South China), Wuhan 430205, China

Received Date: 2022-11-15
Available Online: 2024-10-16
Publish Date: 2024-09-25

Abstract

Abstract

The sedimentary tectonic background of the southeastern part of South China Block (SCB) remains controversial. This study focuses on the set of NE-SW stretching clastic sedimentary with alternating lithology of sand and slate with regional gravel interbeds, conducting the sedimentary strata correlation and detrital zircon U-Pb ages in order to constrain the sedimentary tectonic background. Four Nanhuan-Sinian sedimentary strata sections have been studied and the results show that Nanhuan-Sinian sedimentary of the southeastern part of SCB could be well correlated and provenance with detrital zircon age peak of 900-1 100 Ma migrated from southeast to northwest from the Early Nanhuan to Sinian. "Cathaysia-derived Clastic Strata" are identified according to the lithology and provenance features. The results challenge the opinions that there had been a wide ocean between the blocks of Yangtze and Cathaysia during Nanhuan-Sinian to the west of Zhenghe-Dapu Fault in study area.
- South China Block,
- Nanhuan,
- Sinian,
- stratigraphy correlation,
- detrital zircon provenance,
- stratigraphy,
- sedimentology

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References(141)

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