新疆东天山玉海西岩体地球化学特征及其地质意义

黄宝强; 陈寿波; 李琛; 田庆磊; 王超; 吴见新; 陈明霞; 韩金生; 王云峰

doi:10.3799/dqkx.2018.148

Volume 43 Issue 9

Sep. 2018

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Article Navigation > Earth Science > 2018 > 43(9): 2943-2965

Huang Baoqiang, Chen Shoubo, Li Chen, Tian Qinglei, Wang Chao, Wu Jianxin, Chen Mingxia, Han Jinsheng, Wang Yunfeng, 2018. Geochemical Features and Geological Significance of Yuhaixi Plutons in Eastern Tianshan, Xinjiang. Earth Science, 43(9): 2943-2965. doi: 10.3799/dqkx.2018.148

Citation:

Huang Baoqiang, Chen Shoubo, Li Chen, Tian Qinglei, Wang Chao, Wu Jianxin, Chen Mingxia, Han Jinsheng, Wang Yunfeng, 2018. Geochemical Features and Geological Significance of Yuhaixi Plutons in Eastern Tianshan, Xinjiang. Earth Science, 43(9): 2943-2965. doi: 10.3799/dqkx.2018.148

Citation:

Huang Baoqiang, Chen Shoubo, Li Chen, Tian Qinglei, Wang Chao, Wu Jianxin, Chen Mingxia, Han Jinsheng, Wang Yunfeng, 2018. Geochemical Features and Geological Significance of Yuhaixi Plutons in Eastern Tianshan, Xinjiang. Earth Science, 43(9): 2943-2965. doi: 10.3799/dqkx.2018.148

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Geochemical Features and Geological Significance of Yuhaixi Plutons in Eastern Tianshan, Xinjiang

doi: 10.3799/dqkx.2018.148

1.
No. 704 Geological Party, Xinjiang Geological Exploration Bureau for Nonferrous Metals, Hami 839000, China
2.
Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2018-03-03
Publish Date: 2018-09-15

Abstract

Abstract

The Yuhaixi Mo deposit, located in the eastern part of the Dananhu-Tousuquan island arc belt, was discovered by the No.704 Geological Party of Xinjiang Geological Exploration Bureau for Nonferrous Metals in 2015. Rocks occurring at Yuhaixi contain the Carboniferous Yanchi Formation, Neogene Putaogou Formation and felsic-mafic plutons (gneissic granite, granite, diorite and gabbro dike). LA-ICP-MS zircon U-Pb dating reveals that gneissic granite and diorite replaced at ca. 364 Ma and 306 Ma, respectively. Yuhaixi intrusions are characterized by high ε_Hf(t) (10.5-14.2) and ε_Nd(t) (0.9-4.0) values, and low I_Sr (0.703 282-0.704 111) values, indicating depleted-mantle or juvenile-crust sources. The gneissic granite is characterized by low Mg^# value (22-27), and Zr/Hf (28-33), Ti/Zr (10-29) and Ti/Y (94-149) ratios, implying a juvenile-crust source. The diorite and the gabbro dike are marked by low Si₂O content (47.55%-57.54%), high Mg^# values (51-59), and Ti/Zr (20-380) and Ti/Zr (246-269) ratios, which indicate that these rocks were likely formed by the part melting of the depleted mantle. However, diorite and the gabbro dike samples are rich in LREEs and LILEs (e.g., Rb, Sr), with low Ce/Pb ratios (6.5-12.0), suggesting the mixing of crustal component. Combining with the regional geological studies, the Yuhaixi gneissic granite was likely derived from the juvenile low crust, related with the north subduction of the Kangguer ocean plate; the diorite was also formed under a subducion setting by the partial melting of depleted mantle, and mixed with crustal component when it traversed the crust; the gabbro dike was probably derived from the depleted mantle, mixing with crustal component as well, in a post-collisional extension setting, the age of which was latter than 306 Ma.
- Yuhaixi Mo deposit,
- eastern Tianshan,
- zircon U-Pb dating,
- geochemistry,
- Sr-Nd-Hf isotope

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References(148)

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