新疆西准噶尔早石炭世沉积地层的物源及构造环境

廖婉琳; 肖龙; 张雷; 王国灿

doi:10.3799/dqkx.2015.039

Volume 40 Issue 3

Mar. 2015

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Liao Wanlin, Xiao Long, Zhang Lei, Wang Guocan, 2015. Provenance and Tectonic Settings of Early Carboniferous Sedimentary Strata in Western Junggar, Xinjiang. Earth Science, 40(3): 485-503. doi: 10.3799/dqkx.2015.039

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Liao Wanlin, Xiao Long, Zhang Lei, Wang Guocan, 2015. Provenance and Tectonic Settings of Early Carboniferous Sedimentary Strata in Western Junggar, Xinjiang. Earth Science, 40(3): 485-503. doi: 10.3799/dqkx.2015.039

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Provenance and Tectonic Settings of Early Carboniferous Sedimentary Strata in Western Junggar, Xinjiang

doi: 10.3799/dqkx.2015.039

Liao Wanlin^1
,,
Xiao Long^{1
,
,},
Zhang Lei^{1, 2},
Wang Guocan^{1, 3}

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Hubei Geological and Mining Exploration Limited Liability Company, Wuhan 430022, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-05-07
Publish Date: 2015-03-15

Abstract

Abstract

The geochemistry and detrital zircon characteristics of the sediments play an important role in the study of sedimentary provenance and their tectonic settings. This paper presents petrography and geochemical study of the Early Carboniferous Baogutu Group and Tailegula Group clastic rocks in Karamay area, western Junggar, NW Xinjiang. Geochemical data show that the sedimentary rocks have SiO₂ contents (54.64%-73.14%), relatively high Al₂O₃ contents (11.89%-19.36%) and high (TFe₂O₃+MgO) contents (3.97%-9.99%), indicating low chemical maturity. Their total rare earth element contents vary between 83×10^-6 and 252×10^-6, characterized by no Ce anomaly and slightly negative Eu anomalies, which is similar to those of sandstones formed at oceanic island arc setting. U-Pb dating results of detrital zircons show that Baogutu Group has 340 and 440 Ma two peak values. Detrital zircons of Tailegula Group show only one peak (325 Ma) and suggests that they were sourced from the Early Carboniferous rocks. Discrimination diagrams of the major and trace elements show that the provenance and tectonic settings of Early Carboniferous Baogutu and Tailegula groups sedimentary rocks were formed from the oceanic island arc and continental island arc acidic volcanic rocks, with minor mafic volcanic rocks.
- western Junggur,
- Early Carboniferous,
- geochemistry of sedimentary rock,
- tectonic setting

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References(84)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Provenance and Tectonic Settings of Early Carboniferous Sedimentary Strata in Western Junggar, Xinjiang

doi: 10.3799/dqkx.2015.039

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