西准噶尔谢米斯台地区志留纪中酸性侵入体的成因与构造意义

张叶军; 吕会莉; 王国庆; 李盛富; 杨清茂; 尹松; 杨文龙; 魏虎; 高奇; 郭换青; 李益龙

doi:10.3799/dqkx.2024.131

Volume 50 Issue 8

Aug. 2025

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Article Navigation > Earth Science > 2025 > 50(8): 3013-3033

Zhang Yejun, Lv Huili, Wang Guoqing, Li Shengfu, Yang Qingmao, Yin Song, Yang Wenlong, Wei Hu, Gao Qi, Guo Huanqing, Li Yilong, 2025. Petrogenesis and Tectonic Significance of Silurian Intermediate⁃Acid Intrusive Rocks in the Xiemisitai Area, West Junggar. Earth Science, 50(8): 3013-3033. doi: 10.3799/dqkx.2024.131

Citation:

Zhang Yejun, Lv Huili, Wang Guoqing, Li Shengfu, Yang Qingmao, Yin Song, Yang Wenlong, Wei Hu, Gao Qi, Guo Huanqing, Li Yilong, 2025. Petrogenesis and Tectonic Significance of Silurian Intermediate⁃Acid Intrusive Rocks in the Xiemisitai Area, West Junggar. Earth Science, 50(8): 3013-3033. doi: 10.3799/dqkx.2024.131

Citation:

Zhang Yejun, Lv Huili, Wang Guoqing, Li Shengfu, Yang Qingmao, Yin Song, Yang Wenlong, Wei Hu, Gao Qi, Guo Huanqing, Li Yilong, 2025. Petrogenesis and Tectonic Significance of Silurian Intermediate⁃Acid Intrusive Rocks in the Xiemisitai Area, West Junggar. Earth Science, 50(8): 3013-3033. doi: 10.3799/dqkx.2024.131

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Petrogenesis and Tectonic Significance of Silurian Intermediate⁃Acid Intrusive Rocks in the Xiemisitai Area, West Junggar

doi: 10.3799/dqkx.2024.131

1.
No.216 Team of Nuclear Industry, Urumqi 830011, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Xinjiang Geological Bureau, Urumqi 830000, China

Received Date: 2024-12-13
Publish Date: 2025-08-25

Abstract

Abstract

There are abundant Paleozoic intermediate⁃acid intrusive rocks in the Xiemisitai area, West Junggar, which is a hotspot for the study of crustal accretion of the Central Asian Orogenic Belt. In this study, detailed petrology, geochemistry, zircon U⁃Pb geochronology and Hf isotopic composition analysis were conducted for the intrusive rocks in the Wushijiagayiti gold deposit area in the western section of Xiemisitai. The results show that the intrusive rocks mainly consist of monzonites and quartz monzonites, with zircon U⁃Pb ages ranging from 429 to 424 Ma, ε_Hf(t) values ranging from +11.7 to +15.2, and Hf isotope model ages of t_DM2 of ca. 560 Ma. The monzonites and quartz monzonites have similar geochemical characteristics belonging to high⁃K calc⁃alkaline to shoshonitic series and are enriched in Rb, K, Zr and Hf, depleted Nb, Ta, P and Ti. All of them are typical of I⁃type granitoids and show continental arcaffinity. According to comprehensive research, it is inferred that the intermediate⁃acid intrusive rocks in the western section of the Xiemisitai area were derived from partial melting of young mafic lower crust in a volcanic arc setting during the northward subduction of the Junggar⁃Balkhash Ocean in the early Paleozoic. They recorded the transformation from a basaltic intra⁃oceanic arc to a continental arc during crustal growth.
- intermediate-acid intrusive rocks,
- Xiemisitai volcanic arc,
- magmatism,
- West Junggar,
- Central Asian Orogenic Belt,
- geochemistry

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Petrogenesis and Tectonic Significance of Silurian Intermediate⁃Acid Intrusive Rocks in the Xiemisitai Area, West Junggar

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