地质找矿论丛2013，Vol.28Issue(2)：210-215,6.DOI:10.6053/j.issn.1001-1412.2013.02.007
内蒙古达茂旗满都拉地区铜矿地质特征及找矿方向探讨
Discussion on geological characters and prospecting direction of copper deposit in Mandula area at Damaoqi, Inner Mongolia
摘要
Abstract
Mandula area is situated at Damaoqi-Bainaimiao Cu-Au polymetallic mineralization zone.Paleozoic and Mid-Cenozoic strata are mainly exposed and faults strikes mainly NE,NW and near WE.Late Variscan magmatic rock is dominant.Porphyry,hydrothermal and volcanogenic massive sulfide copper deposits occur in the region.The copper deposits are mainly located in Upper Carboniferous Benbatu formation and Lower Permian Dashizhai formation and controlled by NW and near EW faults.They are closely related to Late Variscan magmatism.Therefore,the EW-trending Upper Carboniferous-Lower Permian volcanic-clastic-carbonate rock series are the target for further prospecting and Late Variscan magmatic rocks and their contact zones with enclosing strata are important prospecting mark.关键词
铜矿床/地质特征/找矿方向/内蒙古达茂旗Key words
copper deposit/ geological characters/ prospecting direction/ Damaoqi/ Inner Mongolia分类
天文与地球科学引用本文复制引用
汤超,陈军强,商志文,李志丹,刘晓雪,任军平..内蒙古达茂旗满都拉地区铜矿地质特征及找矿方向探讨[J].地质找矿论丛,2013,28(2):210-215,6.基金项目
中国地质调查局项目(编号:1212011120721)资助. （编号:1212011120721）
