中天山基底与塔里木克拉通的构造亲缘性

舒良树; 邓兴梁; 马绪宣

doi:10.3799/dqkx.2019.977

Volume 44 Issue 5

May 2019

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Shu Liangshu, Deng Xingliang, Ma Xuxuan, 2019. Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton. Earth Science, 44(5): 1584-1601. doi: 10.3799/dqkx.2019.977

Citation:

Shu Liangshu, Deng Xingliang, Ma Xuxuan, 2019. Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton. Earth Science, 44(5): 1584-1601. doi: 10.3799/dqkx.2019.977

Shu Liangshu, Deng Xingliang, Ma Xuxuan, 2019. Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton. Earth Science, 44(5): 1584-1601. doi: 10.3799/dqkx.2019.977

Citation:

Shu Liangshu, Deng Xingliang, Ma Xuxuan, 2019. Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton. Earth Science, 44(5): 1584-1601. doi: 10.3799/dqkx.2019.977

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Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton

doi: 10.3799/dqkx.2019.977

1.
State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210023, China
2.
Tarim Petroleum Field Prospect Headquarter, Korla 841000, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2019-01-06
Publish Date: 2019-05-15

Abstract

Abstract

The tectonic affinity between the Chinese Central Tianshan basement and the Tarim craton is pivotal for us to understand the tectonic framework of the Central Asian orogenic belt. Based on analyses of field investigation and stratigraphic sequences, it performed detrital zircon U-Pb dating analysis on the four Neoproterozoic meta-sandstone samples from the Gangou region of Hejing County and Alagou region of Baluntai Town, Chinese Central Tianshan. Stratigraphically, the Precambrian strata, rock assemblages, stratigraphical contacts, sedimentary environment in the Chinese Central Tianshan are very similar to those in the northern margin of the Tarim craton, revealing close tectonic affinity between them. All analyzed detrital zircons show oscillatory zoning and have Th/U ratios >0.1 (mainly ranging from 0.4 to 4.0), suggesting that they were mainly derived from igneous rocks. A total of about 165 detrital zircon analyses yielded four age peaks, namely, 950 Ma, 1 550 Ma, 1 920 Ma and 2 480 Ma, respectively, corresponding to four prominent tectonomagmatic events that occurred in the Tarim craton. In addition, these peak ages are remarkably consistent with age populations of detrital zircons in the Tarim craton and its neighbouring areas, and further corroborate that the Chinese Central Tianshan terrane has close tectonic affinity with the Tarim craton. Furthermore, some Proterozoic zircons have been found, showing ages of 2 600-3 260 Ma. Therefore, it is argued that the Chinese Central Tianshan belonged to the Tarim craton in the Precambrian time. Owing to the southward subduction of the Paleo-Tianshan oceanic lithosphere beneath the northern margin of the Tarim craton during the Neoproterozoic period, the remarkable arc-type magmatism occurred in the Chinese Central Tianshan terrane, which rifted away from the Tarim craton.
- stratigraphic sequence,
- detrital zircon,
- U-Pb age population,
- tectonic affinity,
- basement of Chinese Central Tianshan,
- Tarim craton,
- tectonics

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References(68)

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Tectonic Affinity between Central Tianshan Basement and Tarim Block Craton

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