| 抚顺煤田接触热变质带及其煤变质因素分析 |
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| 引用本文： | 庄新国,罗照华.抚顺煤田接触热变质带及其煤变质因素分析[J].地球科学,1994,19(1):82-86. |
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| 作者姓名： | 庄新国 罗照华 |
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| 作者单位： | 中国地质大学矿产系 武汉430074(庄新国),中国地质大学地矿系 北京100083(罗照华) |
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| 摘 要： | 通过对抚顺煤田西露天矿的大比便尺填图以及横向追索,发现大量的接触热变质“烧变煤”的存在,观察到接触热变质带与辉绿岩呈明显的热接触关系。在此基础上,结合岩浆岩研究指出抚顺煤田煤变质为一种具有浅成、高温,作用时间较短的岩浆热变质作用的产物。
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| 关 键 词： | 煤田 热变质带 变质因素 |
Contact Thermal Metamorphic Zones in Fushun Coalfield and Factors for Its Coal Metamorphism |
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| Zhuang Xinguo.Contact Thermal Metamorphic Zones in Fushun Coalfield and Factors for Its Coal Metamorphism[J].Earth Science-Journal of China University of Geosciences,1994,19(1):82-86. |
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| Authors: | Zhuang Xinguo |
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| Abstract: | The discovery of a great quantity of "burnt coal" with contact thermal metamorphism is made possible by large-scale mapping and lateral tracing in the western opencast of Fushun coalfield and a distinct thermal contact relation between the contact thermal metamorphic zones in coal seems and diabases is observed. Along with study of magmatic rocks, the au-thors propose that coal metamorphism in coalfield resulted from shallow magmatic thermal metamorphism with high temperature in a short time. |
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| Keywords: | burnt coal factor for coal metamorphism thermal contact metamorphic zone of coal |
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