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新疆昭苏水磨沟铜金矿特征
引用本文:陶专,何政伟,孙传敏,吴华,刘显凡,吴山,刘兴德,彭方红,王晓地,丁益民.新疆昭苏水磨沟铜金矿特征[J].成都理工大学学报(自然科学版),2002,29(1):85-89.
作者姓名:陶专  何政伟  孙传敏  吴华  刘显凡  吴山  刘兴德  彭方红  王晓地  丁益民
作者单位:成都理工大学地质学系,成都,610059
基金项目:中国地质调查局地质调查项目;200102006300;
摘    要:新疆西天山下石炭统大哈拉军山组地层中产有众多的金矿体。通过对昭苏水磨沟铜金矿床矿化特征的研究 ,总结出这类矿床的成矿规律是 :下石炭统大哈拉军山组中酸性火山岩是矿源层 ;区域性大断裂是矿质运移通道 ,其中的低级别、低序次构造为容矿空间 ;华力西期钾长花岗岩是形成铜金矿的能量来源 ;绿片岩相以下的动力变质作用是矿化富集的条件。矿床成因应属构造破碎蚀变岩型铜金矿床

关 键 词:铜金矿床  矿化特征  成矿规律  找矿标志  水磨沟  新疆
文章编号:1005-9539(2002)01-0085-05
修稿时间:2001年6月12日

GEOLOGICAL CHARACTERISTICS OF THE Cu-Au DEPOSIT IN SHUIMOGOU OF WESTERN XINJIANG, CHINA
TAO Zhuan ,HE Zheng wei ,SUN Chuan min ,WU Hua ,LIU Xian fan ,WU Shan ,LIU Xing de ,PENG Fang hong ,WANG Xiao di ,DIN Yi min.GEOLOGICAL CHARACTERISTICS OF THE Cu-Au DEPOSIT IN SHUIMOGOU OF WESTERN XINJIANG, CHINA[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2002,29(1):85-89.
Authors:TAO Zhuan  HE Zheng wei  SUN Chuan min  WU Hua  LIU Xian fan  WU Shan  LIU Xing de  PENG Fang hong  WANG Xiao di  DIN Yi min
Institution:TAO Zhuan 1,HE Zheng wei 1,SUN Chuan min 1,WU Hua 2,LIU Xian fan 1,WU Shan 1,LIU Xing de 1,PENG Fang hong 2,WANG Xiao di 1,DIN Yi min 1
Abstract:There are many gold deposits occurring in the Dahalajunshan Group of Carboniferous in western Tianshan, Xinjiang, China. Based on the investigations of geological characteristics of the gold and copper deposit in Shuimogou, the metallogenic law of such a deposit can be summarized as follows. Intermediate acid lava in the Dahalajunshan Formation of Carboniferous is the resource bed; Regional faults are the routes of carrying metallogenic elements, in which the little faults are the interspace of containing minerals ; Granite is the energy resource; Dynamical metamorphism under greenschist facies is the condition of mineralizing enrichment. The genesis of the gold deposits of the fragmented altered rock type.
Keywords:Cu  Au deposit  mineralizing characteristics  metallogenic law  ore  search indicator  Shuimogou  Xinjiang
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