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东昆仑东段哈日扎地区含矿斑岩特征及找矿潜力分析
引用本文:韩英善,郭桂兰,张大明,景向阳,奎明娟.东昆仑东段哈日扎地区含矿斑岩特征及找矿潜力分析[J].西北地质,2012,45(1):33-39.
作者姓名:韩英善  郭桂兰  张大明  景向阳  奎明娟
作者单位:青海省第三地质矿产勘查院,青海西宁,810012
基金项目:青海省地质矿产勘查开发局基金项目“青海省都兰县哈日扎地区多金属矿普查”(青地矿[2011]15号)
摘    要:东昆仑东段都兰哈日扎地区出露比较典型的燕山期花岗闪长斑岩,斑岩体以少暗色矿物、多巨斑、石英斑晶具熔蚀现象、普遍见孔雀石化和地表"火烧皮"为特征。斑岩形成于后碰撞伸展构造环境,是加厚陆壳背景环境下的底侵、拆沉构造作用的结果。斑岩具全岩铜矿化特征,属于大陆环境下的斑岩型矿床。从其成矿地质特征、地球物理、地球化学特征和斑岩体深部矿化特征综合分析,该区具有寻找斑岩型铜矿的巨大潜力。

关 键 词:矿斑岩  成矿潜力  哈日扎地区  东昆仑

Characteristics of Ore-Bearing Porphyry and Prospecting Potential Analysis of Harizha in East Kunlun Area
HAN Ying-shan , GUO Gui-lan , ZHANG Da-ming , JIN Xiangyang , KUI Ming-juan.Characteristics of Ore-Bearing Porphyry and Prospecting Potential Analysis of Harizha in East Kunlun Area[J].Northwestern Geology,2012,45(1):33-39.
Authors:HAN Ying-shan  GUO Gui-lan  ZHANG Da-ming  JIN Xiangyang  KUI Ming-juan
Institution:The third geological mineral exploration of Qinghai Province, Xining 810012, China
Abstract:Harizha is located in Dulan in east Kunlun, it developed typical Yanshanian granodiorite-porphy- ry. The porphyry body is characteristic of less melanocratie mineral, giant phenocryst, corroded quartz phenoeryst, widespread malachite mineralization and Fire-skin in surface. Porphyry formed after the colli-sion stretch tectonic environment, is the result of assault and heavy construction effect in the thick conti- nental crust background environment. Porphyry copper deposit with the rock change feature, belongs to the continent in the environment of porphyry deposit, from its metallogenic geological characteristics, geo- physical and geochemical characteristics and deep porphyry mineralization characteristic in the comprehen- sive analysis, it has enormous potential for porphyry copper.
Keywords:ore-bearing porphyry  ore potentials Harizha area east Kunlun
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