摘要
阿舍勒多金属矿田,位于阿舍勒陆缘裂陷槽中。矿田构造为两个复式向斜夹一个复式背斜组成的褶皱束,具有6组断裂,经历了3次拉张,3次闭合的演化历史。矿田地层为泥盆系火山岩建造及下石炭统火山-沉积岩建造。中泥盆世艾菲尔期和晚泥盆世弗拉斯期,为矿田的两个主要成矿期。Ⅰ号矿床形成于艾菲尔期,矿体赋存于古火山机构通道相的次辉绿岩筒筒壁间隙之中。
Ashele multimetal ore field is located at the rift depression of continental margin,characterbod by two synclinoria and one anticlinorium. The six-group fractures in the field show the evolution history of 3-time tension and 3-time closure. The stratigraphy is shown as volcanic formations of Devonian and volcanic-sedimentary formations of Lower Carboniferous. There exist two main ore mineralization stages,i. e,Aifeir stage of Middle Devonian and Feilars stage of Late Devonian. No. 1 ore deposit was formed at the Aifeir stage,with ore body mianly at the in tersetion of sub-diabade cylinder of palaeo-volcanic apparatus phase.
出处
《新疆地质》
CAS
CSCD
1994年第4期351-359,共9页
Xinjiang Geology
关键词
阿舍勒
多金属矿田
地质特征
古火山机构
控矿因素
Ashele, multimetal ore field, geological characteristics,palaeo-volcanic apparatus, ore-controlling factors