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作 者:何以勤 黎原 龚熙珺 陈长江 HE Yi-qin;LI Yuan;GONG Xi-jun;CHEN Chang-jiang(Southern Hunan Institute of Geology and Survey,Chenzhou 423000,China)
出 处:《世界有色金属》2021年第14期223-224,共2页World Nonferrous Metals
摘 要:本区成矿地质条件优越,控矿条件明显,为金属矿矿床。该矿床形成于燕山晚期,经历了从高温-中温-低温的成矿阶段。深边部勘查重点在于突破空白区地段(F4断层西侧),采用就矿找矿原则扩大找矿空间,预期可达超大型矿床以上规模,对矿山开采有一定的指导意义。The metallogenic geological conditions in this area are superior and the ore-controlling conditions are obvious.It is a metallic ore deposit.The deposit was formed in the late Yanshanian period,and experienced the mineralization stage from high temperature to medium temperature to low temperature.The exploration of the deep edge is focused on breaking through the blank area(west of the F4 fault),and using the principle of ore prospecting to expand the ore prospecting space,which is expected to reach the scale of the super-large ore deposit,which has a certain guiding significance for the mine exploitation.
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