内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义

秦锦华; 刘翠; 石玉若; 罗照华; 邓晋福; 李玥霄

doi:10.3799/dqkx.2018.585

Volume 44 Issue 4

Apr. 2019

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Article Navigation > Earth Science > 2019 > 44(4): 1295-1310

Qin Jinhua, Liu Cui, Shi Yuruo, Luo Zhaohua, Deng Jinfu, Li Yuexiao, 2019. Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia. Earth Science, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585

Citation:

Qin Jinhua, Liu Cui, Shi Yuruo, Luo Zhaohua, Deng Jinfu, Li Yuexiao, 2019. Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia. Earth Science, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585

Citation:

Qin Jinhua, Liu Cui, Shi Yuruo, Luo Zhaohua, Deng Jinfu, Li Yuexiao, 2019. Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia. Earth Science, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585

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Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia

doi: 10.3799/dqkx.2018.585

Qin Jinhua^{1,2
,},
Liu Cui^{2
,
,},
Shi Yuruo³,
Luo Zhaohua²,
Deng Jinfu²,
Li Yuexiao²

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

Received Date: 2018-05-21
Publish Date: 2019-04-15

Abstract

Abstract

Genetic types and tectonic backgrounds of miarolitic granite are still controversial. Previous studies have suggested that miarolitic alkali feldspar granites and miarolitic syenite granites belong to A-type granite formed in extensional environment. However, recent studies have found the diversity of the genetic types. In this paper, the petrology, geochemistry and geochronology of Boketu miarolite pluton are present. The zircon SHRIMP U-Pb dating results yield an age of 140.8±2.2 Ma, belonging to the Early Cretaceous. The pluton is characterized by high SiO₂ content, and full high alkali content (7.99%-8.43%), with high K₂O/Na₂O (1.0-1.1); low total Fe content (1.15%-1.30%). On the primitive mantle-normalized spider diagrams, the granite is characterized by positive Th, U, Cs, Rb anomalies and negative Ba, Sr, P, Ti anomalies. 10 000*Ga/Al ratio, the total rare earth content and Zr+Nb+Y+Ce values are lower than the minimum value of the A-type granites. It is indicated that it should belong to Ⅰ-type granite. Hf isotope compositions show the source of juvenile crust. It is mainly restricted by the closure of the Mongolian-Okhotsk ocean, during which the lithosphere transformation from thickening to thinning took place. The granites are formed by the low-degree partial melting of juvenile crust in the underplating of the mantle.
- miarolitic granite,
- Ⅰ-type granite,
- SHRIMP U-Pb dating,
- partial melting,
- petrology

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References(103)

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