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"绿豆岩"组分新析
引用本文:陈忠,唐洪明,沈明道,赵敬松. "绿豆岩"组分新析[J]. 西南石油学院学报, 1999, 21(1): 39-42
作者姓名:陈忠  唐洪明  沈明道  赵敬松
作者单位:西南石油学院勘探系
摘    要:在重庆北碚代家沟乡河犀洞新发现一处厚约1.50m的绿豆岩,豆粒大小为2~5mm。经分离检测分析表明:豆粒存在于伊利石中,伊利石的纯度为95%~97%;对豆粒采用盐酸溶解、X-射线衍射和扫描电镜能谱分析表明:豆粒由石英和方解石组成,石英含量在80%左右,方解石含量约为20%,石英主要分布于豆粒的表面,而方解石则分布于豆粒的中心。

关 键 词:伊利石;绿豆岩;石英;方解石;重庆

NEW ANALYSIS ON THE COMPOSITION OF "MUNG BEAN ROCK"
Chen Zhong,Tang Hongming,Shen Mingdao,Zhao Jingsong. NEW ANALYSIS ON THE COMPOSITION OF "MUNG BEAN ROCK"[J]. Journal of Southwest Petroleum Institute, 1999, 21(1): 39-42
Authors:Chen Zhong  Tang Hongming  Shen Mingdao  Zhao Jingsong
Affiliation:Southwest Petroleum Inst
Abstract:A layer of so-called Mung Bean Rock was recently discovered at Hexidong in Daijiagou, Chongqing. The formation is about 1.5 m thick, in which many hard grains with diameter ranging from 2-5 mm can be easily seen. Compositional analyses show that the rock consists of illitic claystone, with an illite content of 95 -97%. X-ray refraction and SEM examination reveal that the main constituents of the grains are quartz (80%) and calcite (20%). This discovery provides not only a new site to investigate Mung Bean Rock, but also a potential industrial resource of illite.
Keywords:Mung Bean Rock  illite  quartz  calcite  Chongqing
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