重庆桃花赤铁矿矿床主要含矿地层的沉积相分析  

Analysis of sedimentary facies of the main ore bearing strata in the hematite ore deposit, Chongqing

作　　者：刘建伟[1,2] 刘严松[1,2] 李玥[1,2] 王梦潇[1,2] 郝江波[1,2] 

机构地区：[1]国土资源部构造成矿成藏重点实验室(成都理工大学),四川成都610059 [2]成都理工大学地球科学学院,四川成都610059

出　　处：《世界有色金属》2017年第1期202-203,共2页World Nonferrous Metals

摘　　要：重庆桃花赤铁矿大地构造位置处于扬子陆块区-上扬子陆块-南部碳酸盐台地-武隆凹褶束,西侧七曜山断裂带作为川中前陆盆地的分野结构面,成为上扬子陆块古生代坳陷沉积中心。本文主要对矿区的含矿地层的沉积相进行简要的分析。The tectonic position of the peach red hematite in Chongqing is located in the Yangtze Block - the upper Yangtze Block - the southern carbonate platform - Wulong Au fold belt and the Qiyao Mountain fault belt on the west side as the dividing plane structural plane of the central Depositional Center of Paleozoic Depression. In this paper, the sedimentary facies of the ore-bearing strata in the mining area are summarized analyzed.

关 键 词：上泥盆统 含矿层 沉积相 桃花赤铁矿 

分 类 号：P618.45[天文地球—矿床学]