东天山星星峡‒红柳井地区二叠纪A型花岗质岩石成因及构造意义

贺昕宇; 方同辉; 杨自安; 杜海超; 刘海鹏; 王京; 贾润幸; 郑文皓

doi:10.3799/dqkx.2022.241

Volume 49 Issue 9

Sep. 2024

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Article Navigation > Earth Science > 2024 > 49(9): 3089-3105

He Xinyu, Fang Tonghui, Yang Zi'an, Du Haichao, Liu Haipeng, Wang Jing, Jia Runxing, Zheng Wenhao, 2024. Petrogenesis and Tectonic Implications of A-Type Granitoids in the Xingxingxia-Hongliujing Area, Eastern Tianshan. Earth Science, 49(9): 3089-3105. doi: 10.3799/dqkx.2022.241

Citation:

He Xinyu, Fang Tonghui, Yang Zi'an, Du Haichao, Liu Haipeng, Wang Jing, Jia Runxing, Zheng Wenhao, 2024. Petrogenesis and Tectonic Implications of A-Type Granitoids in the Xingxingxia-Hongliujing Area, Eastern Tianshan. Earth Science, 49(9): 3089-3105. doi: 10.3799/dqkx.2022.241

Citation:

He Xinyu, Fang Tonghui, Yang Zi'an, Du Haichao, Liu Haipeng, Wang Jing, Jia Runxing, Zheng Wenhao, 2024. Petrogenesis and Tectonic Implications of A-Type Granitoids in the Xingxingxia-Hongliujing Area, Eastern Tianshan. Earth Science, 49(9): 3089-3105. doi: 10.3799/dqkx.2022.241

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Petrogenesis and Tectonic Implications of A-Type Granitoids in the Xingxingxia-Hongliujing Area, Eastern Tianshan

doi: 10.3799/dqkx.2022.241

He Xinyu^{1, 2, 3, 4
,
,},
Fang Tonghui⁴,
Yang Zi'an⁴,
Du Haichao⁵,
Liu Haipeng⁴,
Wang Jing^{1, 4},
Jia Runxing⁴,
Zheng Wenhao⁴

1.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, China Geological Survey, Wuhan 430205, China
2.
School of Earth Sciences, Institute of Disater Prevention, Sanhe 065201, China
3.
Hebei Key Laboratory of Earthquake Dynamics, Sanhe 065201, China
4.
China Nonferrous Metals Resource Geological Survey, Beijing 100012, China
5.
Geological Corpotation of China Gold Group, Beijing 100012, China

Received Date: 2022-04-06
Available Online: 2024-10-16
Publish Date: 2024-09-25

Abstract

Abstract

Time of terminal accretion of the Central Asian Orogenic Belt (CAOB) is still controversial, and A-type granite in the southern margin of the CAOB can provide critical constraints on the termination of collision. However, the A-type granite in the southern margin of eastern Tianshan remains insufficiently studied. Three kinds of newly identified A-type granitoids, monzogranite, quartz diorite and syenogranite, were reported in this paper and zircon LA-ICP-MS U-Pb dating, trace elements as well as petrogeochemical analysis were conducted. All these granitoids are characterized by high SiO₂ (71.32%-76.35%), alkali (Na₂O+K₂O=5.67%-9.18%), being metaluminous (molar A/CNK=0.85-0.98) and ferroan (FeO^T/MgO=5.52-21.28). The granitoids are enriched in Pb, Hf, Zr, Sm, but depleted in P, Ti, Nb, with high Ga value (18.2×10^-6-31.1×10^-6) and Ga/Al > 2.6. In addition, these granitoids have ΣREE of 77.67×10^-6-271.82×10^-6, LREE/HREE of 2.82-16.26, (La/Yb)_N of 1.80-21.89. Eu anomalies are obviously positive (δEu=0.16-0.84) for both Monzogranite and syenogranite but weakly negative or positive (δEu=0.85-1.20) for the quartz diorite. Monzogranite and syenogranite rather than quartz diorite experienced obvious crystalline fractionation of plagioclase. Monzogranite associated with syenogranite and quartz diorite was also subjected to fractional crystalization of zircon, while the independent one experienced separation of sphene and apatite. Zircon U-Pb dating of monzogranite yields crystallization ages of (273.3±1.9) Ma and (273.4±3.4) Ma. These geochemical features indicate that the primary magma of these A-type granitoids most likely originated from the Xingxingxia complex with minor mantle component, and underwent a fractional crystallization. There exist two distinguished ranges of 307-284 Ma and 273 Ma for A-type granitoids in the Tianshan Orogen, and the elder formed in partial extension environment during the compression period while the younger were emplaced in post-collision background. The eastern section of the southern CAOB had been in post-collision environment in ~273 Ma, and final collision between the eastern section of CAOB and the Tarim Plate should be earlier than 273 Ma.
- eastern Tianshan,
- A-type granite,
- CAOB,
- central Tianshan Orogen,
- Xingxingxia,
- Paleo-Asian Ocean,
- geochemistry,
- petrology

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References(96)

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Petrogenesis and Tectonic Implications of A-Type Granitoids in the Xingxingxia-Hongliujing Area, Eastern Tianshan

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