鄂尔多斯盆地塔然高勒地区直罗组砂岩源区构造背景与物源分析

俞礽安; 朱强; 文思博; 涂家润; 彭胜龙; 司庆红; 唐永香

doi:10.3799/dqkx.2020.001

Volume 45 Issue 3

Mar. 2020

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Article Navigation > Earth Science > 2020 > 45(3): 829-843

Yu Reng'an, Zhu Qiang, Wen Sibo, Tu Jiarun, Peng Shenglong, Si Qinghong, Tang Yongxiang, 2020. Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin. Earth Science, 45(3): 829-843. doi: 10.3799/dqkx.2020.001

Citation:

Yu Reng'an, Zhu Qiang, Wen Sibo, Tu Jiarun, Peng Shenglong, Si Qinghong, Tang Yongxiang, 2020. Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin. Earth Science, 45(3): 829-843. doi: 10.3799/dqkx.2020.001

Citation:

Yu Reng'an, Zhu Qiang, Wen Sibo, Tu Jiarun, Peng Shenglong, Si Qinghong, Tang Yongxiang, 2020. Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin. Earth Science, 45(3): 829-843. doi: 10.3799/dqkx.2020.001

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Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin

doi: 10.3799/dqkx.2020.001

1.
Tianjin Center of China Geological Survey, Tianjin 300170, China
2.
Key Laboratory of Uranium Geology of China Geological Survey, Tianjin 300170, China
3.
Coalfield Geological Bureau of Inner Mongolia, Hohhot 010010, China
4.
Tianjin Geothermal Exploration Institute, Tianjin 300250, China

Received Date: 2019-09-09
Publish Date: 2020-03-15

Abstract

Abstract

Zhiluo Formation is located in Tarangaole area of the Ordos Basin and the research on the provenance and regional sedimentary structural setting remains weak, which restricts the overall evaluation of provenance change of Zhiluo Formationto some extent. Geochemical analysis and zircon U-Pb dating of sandstone in the lower Zhiluo Formation of uranium bearing horizon in Tarangaole area are applied in this paper. The results show that source rocks of the lower part of Zhiluo Formation are mainly felsic sedimentary rocks and few neutral magmatic rocks, and the tectonic setting of which is the active continental margin-continental margin arc environment. Based on the characteristics of trace and rare earth elements and zircon U-Pb dating results, it is considered that the sources of Zhiluo Formation in study area are mainly from Konzite, TTG gneiss, granulite and mafic-ultramafic layered intrusive rocks in Daqingshan-Wulashan area, and Variscan-Indosinian-Yanshanian period magmatic rocks of Yinshan area. The distribution of sandstones in the lower part of Zhiluo Formation clearly reflects the direction of source supply from north to south, the discovery of Triassic detrital zircons indicates that the Indosinian intrusive rocks have been uplifted bare surface to provide material source during the sedimentation of the lower part of Zhiluo Formation in Triassic, and the proportion of younger provenance components in the upper member is higher than that in the lower member of the lower part of Zhiluo Formation.
- Ordos Basin,
- Zhiluo Formation,
- geochemistry,
- zircon U-Pb dating,
- provenance,
- tectonic setting

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References(71)

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Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin

doi: 10.3799/dqkx.2020.001

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