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新疆多拉金矿床成因探讨
引用本文:汪玉珍,刘玉琳.新疆多拉金矿床成因探讨[J].新疆地质,1992(2).
作者姓名:汪玉珍  刘玉琳
作者单位:新疆维吾尔自治区地质矿产局地质矿产研究所 (汪玉珍),新疆维吾尔自治区地质矿产局地质矿产研究所(刘玉琳)
摘    要:从金矿的成矿环境、矿床特征、矿石矿物特点、控矿构造——韧性剪切带特点、同位素特征、流体包裹体特征及黄铁矿化学成分提供的成因信息等,探索多拉金矿的容矿控矿因素、矿质来源和矿液性质,揭示多拉金矿的成因:是受韧性剪切带控制的中低温岩浆热液-变质热液矿床。

关 键 词:多拉  糜棱岩化  韧性剪切带  构造破碎蚀变岩型金矿

GENESIS OF DOLA GOLD DEPOSIT IN XINJIANG
Wang Yuzhen Liu Yuling.GENESIS OF DOLA GOLD DEPOSIT IN XINJIANG[J].Xinjiang Geology,1992(2).
Authors:Wang Yuzhen Liu Yuling
Abstract:The analyses of metallogenic enviroments, ore-controlling structures, ore deposit and its minerals, ductile shearing zone, isotopes, and fluid inclusions, as well as the genetic information provided by chemical compositions of pyrite, are taken to study the ore-containing and ore-controlling factors, the ore resources and the characteristics of ore fluid. It is revealed that the Dola gold deposit is a magmatic-metamorphic hydrothermal deposit of low to intermediate temperature.
Keywords:Dola  mylonitization  ductile shear belt  gold deposit of an alteration type in structural fracture zones  
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