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汝箕沟煤中矿物的成因研究及其意义
引用本文:张慧,李小彦.汝箕沟煤中矿物的成因研究及其意义[J].矿物学报,1993,13(4):362-367.
作者姓名:张慧  李小彦
作者单位:煤炭科学研究总院西安分院,煤炭科学研究总院西安分院 西安 710054,西安 710054
摘    要:本文在较大量和详细的煤岩煤质研究之后,进而用电子探针、扫描电镜及显微镜热台等对宁夏汝箕沟无烟煤中矿物的分成、晶形、微量元素、包裹体温等进行了成因研究。结果表明,汝箕沟煤中的次生矿物及原生矿物的次生变化均与中-低温热液作用有关,这将为该区煤变质成因提供直接证据。

关 键 词:无烟煤  矿物成因论  热液作用  煤系

GENETIC STUDIES OF MINERALS FROM COAL IN RUJIGOU AND THEIR IMPLICATION
Zhang Hui,Li Xiaoyan Central Coal Mining Research Institute,Xi'an Branch,Xi'an.GENETIC STUDIES OF MINERALS FROM COAL IN RUJIGOU AND THEIR IMPLICATION[J].Acta Mineralogica Sinica,1993,13(4):362-367.
Authors:Zhang Hui  Li Xiaoyan Central Coal Mining Research Institute  Xi'an Branch  Xi'an
Institution:Zhang Hui,Li Xiaoyan Central Coal Mining Research Institute,Xi'an Branch,Xi'an,710054
Abstract:On the basis of coal petrology and chemistry, this paper further deals with the composi-tions, crystal forms, trace elements and inclusion temperatures of minerals from anthracite atRujigou, Ningxia, by using electron microprobe (EPA), SEM and thermometry. The resultsshow that the occurrence of secondary minerals and secondary changes of primary mineralsare all related to moderate-low temperature hydrothermal activities. This will provide directevidence for the metamorphogenesis of coal.
Keywords:anthracite  mineral genesis  hydrothermal activity  Ningxia
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