| 河台金矿花岗质糜棱岩显微构造及C面理发育过程 |
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| 引用本文： | 徐霭君,段嘉瑞.河台金矿花岗质糜棱岩显微构造及C面理发育过程[J].中南大学学报(自然科学版),1990(5). |
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| 作者姓名： | 徐霭君 段嘉瑞 |
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| 作者单位： | 中南礦治学院地质系，中南礦治学院地质系 |
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| 摘 要： | 河台金矿花岗质糜棱岩发育良好的糜枝岩面理,表现为石英条带、长石残斑扁平面和石英云母成分层劈理面的平行排列及一组分割性滑移面。它们形成的过程就是矿物显微构造发育过程。
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| 关 键 词： | 显微构造 糜棱岩 面理 石英 长石 云母 金矿/河台 |
THE MICROSTRUCTURE OF GRANITIC MYLONITE AND PROCESS OF C FOLIATION DEVELOPMENT IN HETAI GOLD DEPOSIT |
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| Xu Aijun,Duan Jiarui.THE MICROSTRUCTURE OF GRANITIC MYLONITE AND PROCESS OF C FOLIATION DEVELOPMENT IN HETAI GOLD DEPOSIT[J].Journal of Central South University:Science and Technology,1990(5). |
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| Authors: | Xu Aijun Duan Jiarui |
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| Institution: | Xu Aijun;Duan Jiarui Department of Geology |
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| Abstract: | The well developed foliation of the granite mylonite in Hetai gold deposit
is represented by ribbon of quartz,plaiting surfaces of feldspar prophyro-
clasts,parallelly arranged cleavage planes which are the layer of composition
including quartz and mica.and a set of separated slipping surfaces.The process
of foliation development is just the mineral microstructure development. |
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| Keywords: | miorostructure mylonite foliation quartz mica feldspar gold deposit/Hetal |
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