青海省泽库县电坑金矿区地质特征及找矿前景  

Geological Features and Prospecting of Diankeng Ore Field in Zeku,Qinghai

作　　者：郑崔勇 严琼 艾蒿 李宏鹏 王建良 杨明辉[3] 

机构地区：[1]西北有色地质勘查局711总队,陕西汉中723000 [2]西北有色地质勘查局物化探总队,陕西西安710068 [3]成都理工大学,四川成都610059

出　　处：《甘肃冶金》2016年第2期110-114,118,共6页Gansu Metallurgy

基　　金：中国地质调查局项目<青海省泽库县尼马龙卡-电坑地区金铜钨矿评价>项目编号:12120114003101

摘　　要：工作区位于泽库弧后前陆盆地,在长期沉陷的断陷盆地中沉积的三叠纪古浪堤组成了赋矿地层,构造运动以及印支期中酸性岩浆活动使金富集成矿。区内晚三叠世花岗闪长岩与古浪堤组内外接触带和构造破碎蚀变带中具有寻找构造蚀变岩型金矿的条件。本文初步总结了工作区内的金矿成矿地质背景、找矿标志,根据已发现的找矿线索对找矿前景做以浅析,以期对下一步找矿工作提供借鉴和指导。The survey region is located in foreland basin of the Zeku arc , ore-bearing strata was disposed of Triassic Gulang dikes in long-term subsidence of rift-subsidence basin,gold-rich ore was enriched by the tectonic movement and Indo- Chinese intermediate-acid magmatism. Prospecting condition for structural altered rock type gold deposit exists in Late Tri- assic granodiorite, in Gulang Group contact zone and structure fractured alteration belts. This article sums up the regional gold ore-forming geological background, prospecting according to former clues, and provides reference and guidance for further work.

关 键 词：金矿 构造蚀变岩型 找矿前景 古浪堤组 

分 类 号：P612[天文地球—矿床学] P618.51[天文地球—地质学]