安徽地质Issue(2)：87-91,98,6.
安徽庐枞火山岩盆地西南部“含-横隐伏隆起”构造特征与成矿条件分析
AnAlySiS of StruCturAl feAtureS And ore-formAtion ConditionS of the “hAn-henG hidden uplift” in the SouthweSt of the lu-ZonG volCAniC bASin of Anhui
马冬 1王松根 1吴国荣1
作者信息
- 1. 安徽省地质矿产勘查局326地质队，安徽安庆 246003
- 折叠
摘要
Abstract
“Han-Heng hidden uplift” structure lies in the transitional Hanshan-Hengshan area between “Lu-Zong volcanic basin” and “Indosinian uplift” as a small basement high structure. Recently, a contact-replacement skarn copper-bearing magnetite body was found in the depth of Xiahanshan in the northern part of the uplift. This is a new find in southwestern part of the Lu-Zong volcanic basin for many years and may guide ore exploration in the depth.关键词
含山-横山/隐伏隆起/接触交代矽卡岩/磁铁矿体/成矿条件Key words
Hanshan-Hengshan/hidden uplift/contact-replacement skarn/magnetite分类
天文与地球科学引用本文复制引用
马冬,王松根,吴国荣..安徽庐枞火山岩盆地西南部“含-横隐伏隆起”构造特征与成矿条件分析[J].安徽地质,2015,(2):87-91,98,6.
