CAJ | 학술논문

本文通过实际资料结合已有成果,阐述了贵州大河边一带重晶石矿成矿地质背景,认为在震旦-下寒武早期在该区存在一水下含矿热水喷流隆起带,其严格控制了重晶石矿的产出与分布,在此基础上,总结了该重晶石矿成矿模式,为区内及区域该类型重晶石等矿的潜力评价与勘查提供了新的认识及实践依据。
본문통과실제자료결합이유성과,천술료귀주대하변일대중정석광성광지질배경,인위재진단-하한무조기재해구존재일수하함광열수분류륭기대,기엄격공제료중정석광적산출여분포,재차기출상,총결료해중정석광성광모식,위구내급구역해류형중정석등광적잠력평개여감사제공료신적인식급실천의거。
According to the real information and the exited results,the mineral geologic background in the Dahebian area is discussed,it＇s thought that there is an underwater ore bearing hydrothermal exhalative uplift zone,it controls the outcome and the distribution of the barite deposit.By the discussion,it summarizes the mineral mode of the barite deposit,affords new acknowledgement and practical accordance for the potential judgment and exploration for this kind of barite deposit in this area.