GEOLOGICAL CHARACTERISTICS AND PROSPECTING INDICATORS OF THE KEBULE IRON-COPPER DEPOSIT IN ALXA ZUOQI, INNER MONGOLIA
FENG Ji1, YANG Jian-jun1, LI Peng1,2
1. Key Laboratory of Magmatic Mineralization and Ore-Prospecting, Geological Survey of Inner Mongolia, Hohhot 010020, China; 2. China University of Geosciences, Beijing 100083, China
Abstract：The Kebule Fe-Cu deposit in Alxa Zuoqi, Inner Mongolia, occurs in the external contact zone of the Carboniferous quartz diorite and the second member of Zenglongchang Formation, Zhartaishan Group. The deposit belongs to skarn type, with orebodies hosted in the skarn and surrounding rocks outside the contact zone. The occurrence of the orebodies is consistent with that of the contact zone. The Carboniferous quartz diorite provides the formation of the orebody with heat and materials. In addition, the northeast-trending fractures serve as the pathway for the quartz diorite intrusion and ore-forming fluid. Based on the analysis of the metallogenic geological characteristics, the authors summarize the comprehensive prospecting indicators.
冯骥, 杨建军, 李鹏. 内蒙古阿拉善左旗克布勒铁铜矿地质特征及找矿标志[J]. 地质与资源, 2017, 26(4): 353-356.
FENG Ji, YANG Jian-jun, LI Peng. GEOLOGICAL CHARACTERISTICS AND PROSPECTING INDICATORS OF THE KEBULE IRON-COPPER DEPOSIT IN ALXA ZUOQI, INNER MONGOLIA. GEOLOGY AND RESOURCES, 2017, 26(4): 353-356.
2017, Vol. 26 
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