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煤的岩浆热变质作用
引用本文:吴传荣.煤的岩浆热变质作用[J].煤田地质与勘探,1992,20(4):24-30.
作者姓名:吴传荣
作者单位:煤炭科学研究总院西安分院 710054
摘    要:根据国内外资料,概括总结了岩浆热变质作用的煤质特征、煤牌号带状分布的规律,以及岩浆热变质作用的成因标志。此外,还重点探讨岩浆热变质作用的形成机理,提出了一个新的岩浆热变质作用的地质模式,即热源(岩浆)-储热体系-地热异常区-煤的变质带。这一观点特别强调热源(岩浆)与地质边界条件的相互关系,并认为此乃造成煤变质差异的重要原因。 

关 键 词:岩浆热变质作用    热源/岩浆    储热体系    地热异常区    煤变质带
收稿时间:1992-03-08

MAGMATIC THERMO-METAMORPHISM OF COAL
Wu Chuanrong.MAGMATIC THERMO-METAMORPHISM OF COAL[J].Coal Geology & Exploration,1992,20(4):24-30.
Authors:Wu Chuanrong
Institution:Xi'an Branch, CCMRI
Abstract:According to a series of domestic and foreign reference materials, the paper summarizes the properties of coal quality for magmatic thermo-metamorphism; coal zonal distribution regularity; and the genesis indication for magmatic thermo-metamorphism. Moreover, the paper emphatically analyse the formative mechanism on magmatic thermo-metamorphism, The author points out new type of geological pattern for magmatic thermo-metamorphism, it may be described as follows, heater (magmatic)-heat collecting system-geothermally disturbed area- coal metamorphic zones, this viewpoint especially emphasizes the interrelation between heater (magmatic) and geologic boundary condition, and make sure is an important reason for causing coal metamorphic difference. 
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