北阿尔金野马泉二长花岗岩成因及其构造意义

郑坤; 吴才来; 郜源红; 郭文峰; 陈红杰; 吴迪; 高栋

doi:10.3799/dqkx.2018.719

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1266-1277

Zheng Kun, Wu Cailai, Gao Yuanhong, Guo Wenfeng, Chen Hongjie, Wu Di, Gao Dong, 2018. Petrogenesis and Tectonic Implications of Yemaquan Monzogranite from North Altyn. Earth Science, 43(4): 1266-1277. doi: 10.3799/dqkx.2018.719

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Zheng Kun, Wu Cailai, Gao Yuanhong, Guo Wenfeng, Chen Hongjie, Wu Di, Gao Dong, 2018. Petrogenesis and Tectonic Implications of Yemaquan Monzogranite from North Altyn. Earth Science, 43(4): 1266-1277. doi: 10.3799/dqkx.2018.719

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Petrogenesis and Tectonic Implications of Yemaquan Monzogranite from North Altyn

doi: 10.3799/dqkx.2018.719

Zheng Kun^{1,2
,},
Wu Cailai^{1
,
,},
Gao Yuanhong¹,
Guo Wenfeng¹,
Chen Hongjie¹,
Wu Di³,
Gao Dong¹

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

Yemaquan monzogranite pluton is the largest outcrop in North Altyn, with a medium-coarse grain and porphyritic texture. This paper aims to discuss the genesis and diagenesis environment of the monzogranite, and the tectonic evolution of North Altyn. Thus, it is necessary to study petrology, geochemistry, zircon U-Pb chronology and Hf isotope of the pluton. The zircon U-Pb age data suggest that the monzogranite was generated at 450-453 Ma. The rock shows significant features of Ⅰ-Type granite with high ratio of Na₂O/K₂O (1.72-2.29), aluminum saturation index (A/CNK=0.99-1.10) and negative correlation between P₂O₅% and SiO₂%. The REE pattern shows depletion of HREE, relative enrichment of LREE, and slightly negative Eu anomaly. In the primitive mantle-normalized trace-element diagram, the rock shows strong enrichment of Rb, Ba, Th, U, K and depletion of Nb, Ta, P, Ti. The values of ε_Hf(t) range in 5.52-10.75. The two-stage model ages (t_DM2) vary from 0.75 to 1.09 Ga. These characteristics indicate that the source rock was formed from the juvenile crust (basites). Considering the regional tectonic setting, it is concluded that the monzogranite was generated by partial melting of the basites at the root of the orogenic belt in the syn-collision to post-collision environment.
- monzogranite,
- geochemistry,
- U-Pb chronology,
- Hf isotopic characteristics,
- petrogenesis,
- North Altyn

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References(79)

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