江西金滩岩体花岗岩的侵位深度——来自白云母矿物化学成分的约束-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

江西金滩岩体花岗岩的侵位深度——来自白云母矿物化学成分的约束

The emplaced depth of the granite from Jintan pluton: Constraints from mineral chemistry of muscovite

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DOI	10.20086/j.cnki.yskw.2024.0404
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2024, 43(4)
作者	陶继华，杨跃贵，张吉源，石争，许德如,
作者单位	1. 东华理工大学地球科学学院, 江西南昌 330013; 2. 东华理工大学核资源与环境国家重点实验室, 江西南昌 330013; 3. 东华理工大学江西省大气污染成因与控制重点实验室, 江西南昌 330013
摘要	白云母是过铝质花岗岩中常见的矿物,可以用来作为限制岩体侵位深度的压力计矿物。文章利用电子探针对金滩二云母花岗岩中的白云母进行了化学成分分析,通过白云母结晶压力计算获得金滩岩体的侵位压力为4.9×10⁸~6.1×10⁸ Pa,平均5.4×10⁸ Pa,对应的侵位深度为16~20 km,平均18 km。综合前人研究成果认为,华南印支期花岗岩侵位深度普遍为17~19 km,且华南印支期造山加厚的地壳厚度很可能≥50 km,而在燕山期经历了强烈的风化剥蚀去顶作用。这一认识为揭示华南地区相对缺乏印支期火山岩提供了一种新的解释。
Abstract	Muscovite is a common mineral in peraluminous granites, it could be a mineral barometer to constrain the emplacement depth of peraluminous granites. Chemical compositions of muscovite from the Jintan two-mica granite are determined using electron microprobe. According to the calculation for the crystallization pressure of the muscovite, the pressure of emplacement of the Jintan pluton is 4.9×10⁸~6.1×10⁸ Pa with average 5.4×10⁸ Pa, corresponding to 16~20 km with average 18 km in depth. Combing with previous studies, we suggest that the emplace depth is 17~19 km, and we can presume that crustal thickness of South China in the Indosinian period was likely ≥50 km, but it may be denudated because of extensive weathering in the Yanshanian period, which can be a new explanation for the lacking Indosinian volcanic rocks in South China.
关键词	华南；花岗岩；金滩岩体；白云母；侵位深度
KeyWord	South China; granite; Jintan pluton; muscovite; emplace depth
基金项目
页码	847-855

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陶继华，杨跃贵，张吉源，石争，许德如. 江西金滩岩体花岗岩的侵位深度——来自白云母矿物化学成分的约束 [J]. 岩石矿物学杂志. 2024; 43; (4). 847 - 855.

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