新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2015年
1期
73-77
,共5页
克细克红那海%银铜矿%地质特征%成因初探
剋細剋紅那海%銀銅礦%地質特徵%成因初探
극세극홍나해%은동광%지질특정%성인초탐
Kexikehongnahai%Silver copper mine%Geological characteristics%Gensis preliminary investigate
克细克红那海银铜矿位于阿吾拉勒-伊什基里克金、银、铜、铅、锌（铁）锰成矿带西段，成矿地质条件优越。通过对矿床地质特征及成因的初步总结分析，认为矿化赋存与下石炭统大哈拉军山组第三段玄武粗面安山岩、粗面安山岩、凝灰质砂岩中，受近EW向和近NS向断裂控制，经多期热液成矿作用叠加成矿，属中低温热液充填型矿床。
剋細剋紅那海銀銅礦位于阿吾拉勒-伊什基裏剋金、銀、銅、鉛、鋅（鐵）錳成礦帶西段，成礦地質條件優越。通過對礦床地質特徵及成因的初步總結分析，認為礦化賦存與下石炭統大哈拉軍山組第三段玄武粗麵安山巖、粗麵安山巖、凝灰質砂巖中，受近EW嚮和近NS嚮斷裂控製，經多期熱液成礦作用疊加成礦，屬中低溫熱液充填型礦床。
극세극홍나해은동광위우아오랍륵-이십기리극금、은、동、연、자（철）맹성광대서단，성광지질조건우월。통과대광상지질특정급성인적초보총결분석，인위광화부존여하석탄통대합랍군산조제삼단현무조면안산암、조면안산암、응회질사암중，수근EW향화근NS향단렬공제，경다기열액성광작용첩가성광，속중저온열액충전형광상。
Kexikehongnahai silver copper deposit is located in the Awulale-Yishengjilike gold, silver,copper,lead,zinc (iron) west of manganese metallogenic belt,metallogenic geological condition is superior.Through the preliminary sum-many of the geological characteristics of the deposit and cause analysis,The mineralization occurs and the lower Carbon-iferous Dahalajunshan group third basaltic trachyte andesite,trachyandesite section,tuffaceous sandstone,the orebody is controlled by E-W and S-N trending faults control,after multi-phase superimposed hydrothermal mineralization,the orebody belongs to meso epithermal filling type.
