Genesis of Huogeqi copper-polymetallic deposit in the northern margin of the North China Craton related to Orogenic-type deposit:Evidence from Fe,S,O,H isotope

摘要：

　　The genetic controversy of the Huogeqi copper-polymetallic deposit,located in the northern margin of the North China Craton (NCC) have long affected geologists prospecting.All orebodies of the deposit are enclosed within shear zone.The most popular exhalative-sedimentary model proposed for the Huogeqi deposit (Peng et al.,2006,2007) stresses that the deposit was deposited simultaneously with its host rocks and later underwent metamorphism,deformation and a limited degree of magmatic hydrothermal overprinting (Pi et al.,2010).

作者: Qiao-Hui Pi

作者单位: Guilin University of Technology,Guilin 541004,China

会议类型: 国际会议

会议名称: 第十二届镍矿床国际会议

会议地点: 贵阳

会议语种:英文

页码: 277-277

在线出版日期: 2012-06-16（万方平台首次上网日期，不代表论文的发表时间）