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四川平武绿柱石宝石成矿地质特征
引用本文:周开灿,亓利剑,向长金,冯启明,万吉善,郝芹.四川平武绿柱石宝石成矿地质特征[J].矿物岩石,2002,22(4):1-7.
作者姓名:周开灿  亓利剑  向长金  冯启明  万吉善  郝芹
作者单位:1. 西南科技大学,四川,绵阳,621002
2. 中国地质大学珠宝学院,湖北,武汉,430074
3. 西南核物理与化学研究所,四川,绵阳,621000
4. 绵阳市质检所,四川,绵阳,621000
基金项目:国家自然科学基金项目 (19772 0 96),绵阳市科学基金项目资助成果
摘    要:四川平武产出世界上十分稀少和珍贵的无色透明扁平板状绿柱石宝石。在野外详细调研和系统分析、测试基础上,全国总结和介绍矿床成矿地质环境,绿柱石宝石产出特征,绿柱石宝石矿物学、化学成分、结晶习性及晶体化学、谱学特征、包裹体特征,花岗岩与Be及W,Sn矿化关系和成矿的物理、化学条件。从而,确认该矿床为岩浆期后气成-热液型绿柱石宝石矿床。

关 键 词:绿柱石宝石  成矿地质特性  矿床成因  四川  晶体化学  结晶习性  包裹体
文章编号:1001-6872(2002)04-0001-07
修稿时间:2002年3月19日

GEOLOGIC CHARACTERISTIC OF FORMING BERYL GEM FORM PINGWU SICHUAN
ZHOU Kai can ,QI Li jian ,XIANG Chang jin ,FENG Qi ming ,WU jie shan ,HAO Qing .Southwest University of Science and Technology,Mianyang ,China,.Jevelry Institute of Chinese Geology University,Wuhan , .Southwest Institute of Nuclear Physics and Chemistry,Mianyang ,China, .Production Quality Supervisory Institute of Mianyang,Mianyang ,China.GEOLOGIC CHARACTERISTIC OF FORMING BERYL GEM FORM PINGWU SICHUAN[J].Journal of Mineralogy and Petrology,2002,22(4):1-7.
Authors:ZHOU Kai can  QI Li jian  XIANG Chang jin  FENG Qi ming  WU jie shan  HAO Qing Southwest University of Science and Technology  Mianyang  China  Jevelry Institute of Chinese Geology University  Wuhan  Southwest Institute of Nuclear Physics and Chemistry  Mianyang  China  Production Quality Supervisory Institute of Mianyang  Mianyang  China
Institution:ZHOU Kai can 1,QI Li jian 2,XIANG Chang jin 3,FENG Qi ming 1,WU jie shan 4,HAO Qing 4 1.Southwest University of Science and Technology,Mianyang 621002,China,2.Jevelry Institute of Chinese Geology University,Wuhan 430074, 3.Southwest Institute of Nuclear Physics and Chemistry,Mianyang 621002,China, 4.Production Quality Supervisory Institute of Mianyang,Mianyang 621000,China
Abstract:The colorless transparent flat tabular beryl gem of Pingwu County,Sichuan Province is rare and valuable in the world. The paper comprehensively summaried and introduced the geologic characteristics of deposits, the mineralogy of beryl gem and the physical and chemical condition of mineralization.It was considered the postmagmatic pneumatolito hydrothermal solution was reponsible for the formation of the beryl gem deposit.
Keywords:beryl gem  metallogenetic  characteristics  genesis of ore deposit  Pingwu Sichuan
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