苏克塔格能厄肯红柱石矿床地质特征  

Geological features of geological deposits in SukkerTaggnenEken

作　　者：杨海英[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第三地质大队,新疆库尔勒841000

出　　处：《新疆地质》2013年第1期34-36,共3页Xinjiang Geology

摘　　要：苏克塔格能厄肯红柱石矿床位于新疆库尔勒市境内,大地构造位置处于南天山冒地槽褶皱带霍拉山复向斜东部,南邻塔里木地台库车凹陷,是苏克塔格能厄肯-玉奇阿恰红柱石成矿带中的红柱石矿床之一。区内褶皱、断裂、岩浆岩发育,矿床产于中上石炭统塔拉克组中。经长期地质研究认为:该矿床成因属较浅部高温低压接触变质型红柱石矿床。The Sukker Taggnen Eken andalusite deposit is located within the Korla City.Mine tectonic position is located in eastern Hora Mountain synclinorium of geosyncline fold belt over southern Tianshan top,the south of which is adjacent to Kuqa Depression of Tarim Platform,that is also one of andalusite deposit in SukkerTaggnenEken-Yu Qi Eqia andalusite metallogenic belt.Folds fractures and magmatic rocks also grow in this region.The deposits produce in a formation of Middle and Upper Carboniferous Tarlac group.After a long period of geological study geological features,magmatic rock characteristics,structural characteristics,concluded as follows：The GENESIS is the shallower parts of the hightemperature low-pressure contact metamorphic andalusite mine.

关 键 词：苏克塔格能厄肯 红柱石矿床 地质特征 

分 类 号：P619.2[天文地球—矿床学]