作　　者： (谭丰羽）; (牛泽华）;

机构地区： 成都理工大学地球科学学院,四川成都610059

出　　处： 《云南化工》 2017年第8期109-111,共3页

摘　　要： 额敏县克孜勒乔克地区位于准噶尔盆地西北边缘,塔额盆地东北部,额敏河上游一带,属中高山区,地势总体北高南低,地形切割较强烈,为中-强切割区,是重要的金、铜、铁等矿床的富集区域。本研究就该地区的变质岩特征进行较为系统的阐述。 The Kizilqiaokou area is located in the northeastern edge of the Junggar Basin, northeast of the Tarim Basin, and the upper reaches of the Emin River. It belongs to the submountainous area.In general, the terrain is lower in the north and higher in the south.The stronger topographical segmentation is a area of moderate intensity and crucial region full of gold 、 copper、 iron and other deposits.The characteristics of metamorphic rocks in this area are systematically stated in this research.

关 键 词： 构造旋回 变质作用 矿物共生组合