太行山南段教场闪长岩矿物学特征及其地质意义

史志伟; 董国臣; 高庭; 刘延畅; 宋卡迪

doi:10.3799/dqkx.2019.210

Volume 45 Issue 6

Jun. 2020

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Shi Zhiwei, Dong Guochen, Gao Ting, Liu Yanchang, Song Kadi, 2020. Mineralogical Characteristics of Jiaochang Diorite in Southern Taihang Mountains and Geological Significance. Earth Science, 45(6): 2103-2116. doi: 10.3799/dqkx.2019.210

Citation:

Shi Zhiwei, Dong Guochen, Gao Ting, Liu Yanchang, Song Kadi, 2020. Mineralogical Characteristics of Jiaochang Diorite in Southern Taihang Mountains and Geological Significance. Earth Science, 45(6): 2103-2116. doi: 10.3799/dqkx.2019.210

Citation:

Shi Zhiwei, Dong Guochen, Gao Ting, Liu Yanchang, Song Kadi, 2020. Mineralogical Characteristics of Jiaochang Diorite in Southern Taihang Mountains and Geological Significance. Earth Science, 45(6): 2103-2116. doi: 10.3799/dqkx.2019.210

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Mineralogical Characteristics of Jiaochang Diorite in Southern Taihang Mountains and Geological Significance

doi: 10.3799/dqkx.2019.210

Shi Zhiwei^{1
,
,},
Dong Guochen^{1
,
,},
Gao Ting²,
Liu Yanchang³,
Song Kadi⁴

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Guangdong Institute of Eco-Environmental Science & Technology, Guangzhou 510650, China
3.
Office of the CPC Committee, Beijing University of Technology, Beijing 100124, China
4.
School of Information Science and Technology, Northwest University, Xi'an 710127, China

Received Date: 2019-05-05
Publish Date: 2020-06-15

Abstract

Abstract

The petrogenesis and evolution of Mesozoic complex in the southern Taihang Mountains have been one of hot topics explored since last several decades. Based on field investigation and Electron Probe Microanalysis (EPMA), in the paper, it studies the mineralogy and its significance of Jiaochang diorite. The Jiaochang diorite is mainly composed of plagioclase, amphibole, biotite, and few clinopyroxene and olivine. The SiO₂ contents of the rocks range from 52.91% to 53.39% with high Mg^# [100×Mg/(Mg+Fe²⁺)] (60.28-62.39) and Na (Na₂O/K₂O=1.18-1.40). The plagioclases (about 50%) present An number of 36 to 60 with normal zoning, and belong to andesine and labradorite. The amphiboles (about 30%) has high CaO (>10%) and MgO (>18%), belonging to magnesial amphibole. With [Mg/(Mg+Fe²⁺+Fe³⁺+Mn)] of 0.564-0.582, the biotite (about 12%) is magnesial. The clinopyroxenes (about 5%) belong to Ca-Mg-Fe pyroxene series, which were produced by gradual crystallization of mantle-derived magma during its upwelling from deep to shallow. The olivines (about 2%) as xenocrysts are composed of chrysolite and forsterite with Fo from 76 to 91. The crystallized temperature and pressure of the diorite by clinopyroxene geothermobarometry range from 1 060 ℃ to 1 094 ℃ and from 0.24 GPa to 0.55 GPa respectively. These characteristics suggest that the diorite formed by mantle derived materials from the magma sources. The magma had almost no differentiation during the upward process and the diorite reflects the dual tectonic background of the subduction of the ancient Pacific plate and the extension of North China craton.
- EPMA,
- geothermometer,
- olivine xenocryst,
- diorite,
- southern Taihang Mountains,
- petrology

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References(112)

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Mineralogical Characteristics of Jiaochang Diorite in Southern Taihang Mountains and Geological Significance

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