准噶尔盆地东北缘卡拉麦里组物源区特征:碎屑岩地球化学及锆石U-Pb年代学的制约

白建科; 陈隽璐; 朱小辉; 冯博

doi:10.3799/dqkx.2018.587

Volume 43 Issue 12

Dec. 2018

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Article Navigation > Earth Science > 2018 > 43(12): 4411-4426

Bai Jianke, Chen Junlu, Zhu Xiaohui, Feng Bo, 2018. Provenance Characteristics of Kalamaili Formation in Northeastern Margin of Junggar Basin: Constraints of Geochemistry and Detrital Zircon U-Pb Geochronology. Earth Science, 43(12): 4411-4426. doi: 10.3799/dqkx.2018.587

Citation:

Bai Jianke, Chen Junlu, Zhu Xiaohui, Feng Bo, 2018. Provenance Characteristics of Kalamaili Formation in Northeastern Margin of Junggar Basin: Constraints of Geochemistry and Detrital Zircon U-Pb Geochronology. Earth Science, 43(12): 4411-4426. doi: 10.3799/dqkx.2018.587

Citation:

Bai Jianke, Chen Junlu, Zhu Xiaohui, Feng Bo, 2018. Provenance Characteristics of Kalamaili Formation in Northeastern Margin of Junggar Basin: Constraints of Geochemistry and Detrital Zircon U-Pb Geochronology. Earth Science, 43(12): 4411-4426. doi: 10.3799/dqkx.2018.587

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Provenance Characteristics of Kalamaili Formation in Northeastern Margin of Junggar Basin: Constraints of Geochemistry and Detrital Zircon U-Pb Geochronology

doi: 10.3799/dqkx.2018.587

Bai Jianke^{1,2
,},
Chen Junlu^1,2,
Zhu Xiaohui^1,2,
Feng Bo^1,3

1.
Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
2.
Orogen Research Center, China Geological Survey, Xi'an 710054, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2018-03-10
Publish Date: 2018-12-15

Abstract

Abstract

The Devonian Kalamaili Formation is widely exposed in the northeastern margin of Junggar basin, while its depositional age and tectonic setting are still in debate. In this study, an integrated analysis of petrology, geochemistry and isotope chronology for the Kalamaili Formation was carried out. The results show that the Kalamaili Formation, characterized by turbidite features, was mainly deposited in the slope and semi-deep ocean. Geochemically, the Kalamaili Formation sandstone is characterized by high SiO₂, low Al₂O₃/SiO₂ and high K₂O/Na₂O. The REE distributing patterns show rightward incline and weaker negative Eu anomaly (ΣLREE/ΣHREE=4.81-8.03, δEu=0.59-0.80). Tectonic-setting discrimination diagrams of the Kalamaili Formation sandstone indicate a passive-margin tectonic setting. The detrital zircon age spectrum of the Kalamaili Formation sandstone was composed of two age groups, including 393-524 Ma and 823-3 077 Ma, which correspond to the Early Paleozoic orogenic belt and Precambrian crystalline basement of Junggar basin, respectively. It is concluded that the Kalamaili Formation was deposited in a passive-margin of the northeastern Junggar block during the Early-Middle Devonian.Since the Middle Devonian, the Paleozoic Kalamaili Ocean subducted northward continuously, and then formed the Yemaquan island arc and related forearc sedimentary system, and finally the Kalamaili Ocean closed prior to the Early Carboniferous.
- northeastern margin of Junggar basin,
- Kalamaili Formation,
- detrital zircon,
- passive continental margin,
- geochemistry

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References(77)

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Provenance Characteristics of Kalamaili Formation in Northeastern Margin of Junggar Basin: Constraints of Geochemistry and Detrital Zircon U-Pb Geochronology

doi: 10.3799/dqkx.2018.587

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