摘要
通过对重庆市綦江篆塘角铁矿矿床地质、矿体规模及形态的特征分析,初步研究认为,该矿床属于"綦江式"铁矿,而其成因类型属内陆湖沼相沉积。
The Zhuantangjiao Fe deposit is located in the Dongxi anticline and confined to the first Member of the Lower Jurassic Zhenzhuchong Formation. Two orebodies have been found and occur as lens. Geological characteristics indicate that the deposit belongs to the Qijiang-type one which was formed in an inland limnetic environment.
出处
《四川地质学报》
2009年第2期149-152,161,共5页
Acta Geologica Sichuan
关键词
地质特征
成因
綦江式铁矿
重庆綦江
geological feature
genesis
Qijiang-type Fe deposit
Qijiang, Chongqing
