辽西地区夕卡岩型铁矿成矿规律及找矿方向探讨  

METALLOGENIC REGULARITY AND PROSPECTING GUIDE OF THE SKARN-TYPE IRON DEPOSIT IN WESTERN LIAONING PROVINCE

作　　者：任群智[1] 姚玉增[1] 金成洙[1] 

机构地区：[1]东北大学地质系,辽宁沈阳110004

出　　处：《地质与资源》2009年第4期265-269,共5页Geology and Resources

基　　金：辽宁省自然科学基金项目(20072029)资助

摘　　要：辽西地区分布有巨厚的碳酸盐建造,其与中生代中酸性岩浆岩体相互接触形成了较多的夕卡岩铁矿.该类型矿床多产于辽西台陷与山海关台拱接触部位,与镁夕卡岩关系密切,多与铅、锌、钼等金属密切伴生.结合区域地球物理及地球化学资料,圈定大屯和钢屯偏道子为本区夕卡岩铁矿的成矿远景区.Large-scaled carbonate formation is distributed in Western Liaoning Province. Along the contact zone of the carbonate formation and Mesozoic acid-intermediate magmatic rock bodies, occur lots of skarn-type iron ore deposits. Most of them, intimately related to Mg-skarn, form in the inter-terrestrial part between Western Liaoning syneclise and Shanhaiguan anteclise, coexisting with Pb, Zn, Mo etc. Combined with regional geophysical and geochemical data, the Datun and Piandongzi areas are regarded as advantageous prospecting targets.

关 键 词：夕卡岩型铁矿 成矿规律 找矿方向 辽西地区 

分 类 号：P618.31[天文地球—矿床学]