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多罗山钨矿床黑钨矿晶体形貌学研究
引用本文:王文魁,甘正梅.多罗山钨矿床黑钨矿晶体形貌学研究[J].地球科学,1992,17(6):638-646.
作者姓名:王文魁  甘正梅
作者单位:中国地质大学地质系 (王文魁,王根元),广东多罗山钨矿(甘正梅)
摘    要:简要论述了典型热液裂隙充填钨—铋—钼石英脉矿床地质及其以黑钨矿—辉铋矿—辉钼矿为主的矿物组合纵向逆分带现象。重点测量研究了黑钨矿晶体的宏观形态特征和微形貌,及其成因演化机制。以现代光学微分干涉(DIC)显微镜观察测量了黑钨矿端面(102)等的螺旋生长及010]晶带等的层生长现象。提出黑钨矿晶体的螺—层混合生长概念。

关 键 词:钨矿床  黑钨矿  晶体  形态学

THE MORPHOLOGICAL STUDY OF WOL- FRAMITE , DUOLUOSHAN W -DEPOSIT, GUANGDONG PROVINCE
Wang Wenkui Wang Genyuan.THE MORPHOLOGICAL STUDY OF WOL- FRAMITE , DUOLUOSHAN W -DEPOSIT, GUANGDONG PROVINCE[J].Earth Science-Journal of China University of Geosciences,1992,17(6):638-646.
Authors:Wang Wenkui Wang Genyuan
Abstract:The paper discusses the hydrothermal filling deposit of W-Bi-Mo quartz vein type and the vertical reverse zoning distribution of wolframite-bismuthinite- molybdenite mineral group .More detail studies of both macro -shape and micromorphological characteristics of wolframite crystals with goniometer and differential interference contrast (DIC) microscope are made . Several DIC photos served as criteria to the spiral -layer combined growth mechanism of wolframite .
Keywords:wolframite  crystal morphology  differential interference contrast (DIC) microscope  spiral-layer combined growth mechanism  
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