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陕川丁家林-太阳坪金矿床黄铁矿标型特征
引用本文:刘爽,刘新会,魏宽义.陕川丁家林-太阳坪金矿床黄铁矿标型特征[J].地质找矿论丛,2005,20(Z1):20-23.
作者姓名:刘爽  刘新会  魏宽义
作者单位:1. 武警黄金部队,第五支队,西安,710010
2. 长安大学,地球科学与国土资源学院,西安,710054
摘    要:金矿床中黄铁矿的化学元素、晶体形态、粒度等标型特征与其形成的物理化学环境及介质条件密切相关.通过对陕川丁家林-太阳坪金矿区主要载金矿物黄铁矿在韧性剪切变形-构造分异热液期与脆性剪切变形-构造分异热液期化学元素含量对比,以及黄铁矿形态、粒度分析,研究黄铁矿与金矿物关系.丁家林-太阳坪金矿黄铁矿形态以{100}、{210}单晶及{100} {210}聚晶为其标型.黄铁矿在空间分布特征来看,深部成矿的可能性不大.应沿丁家林-太阳坪脆-韧性剪切带寻找金矿.

关 键 词:黄铁矿  微量元素  形态  热液期  变质期  陕西  四川
文章编号:1001-1412(2005)S0-0020-04
修稿时间:2005年3月18日

CHARACTERISTICS OF TRACE ELEMENTS, PYROELECTRICITY AND CRYSTAL FORM OF PYRITES FROM DINGJIALIN-TAIYANGPING GOLD DEPOSITS IN THE SHAANXI-SICHUAN BORDER AREA
LIU Shuang,LIU Xin-hui,WEI Kuan-yi.CHARACTERISTICS OF TRACE ELEMENTS, PYROELECTRICITY AND CRYSTAL FORM OF PYRITES FROM DINGJIALIN-TAIYANGPING GOLD DEPOSITS IN THE SHAANXI-SICHUAN BORDER AREA[J].Contributions to Geology and Mineral Resources Research,2005,20(Z1):20-23.
Authors:LIU Shuang  LIU Xin-hui  WEI Kuan-yi
Abstract:Typomorphic characteristics of pyrites in Au deposits, such as chemical elements, pyroelectricity and crystal form are closely related to the physio-chemical conditions under which they were formed. This paper deals with relation of pyrite to Au minerals in Dingjialin-Taiyangping Au deposit according to the chemical analysis of elements in gold -bearing pyrites formed in the ductile deformation-tectonic differentiation hydrothermal and the brittle deformation-tectonic differentiation hydrothermal stage respectively and their morphologes and grain sizes. Single crystals with {100}, {210} and polycrystals with {100}+{210} are typomorphology of pyrite in Dingjialin-Taiyangping Au deposit. The relation shows that ore formation is unlite to depth thus further exploration should be along Dingjialin-Taiyangping britlle-ductile shear zone.
Keywords:pyrie  micro-element  morphology  hydrothermal stage  searching for ore along shear zone  Shaaxi province  Sichuan province
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