摘要
杨梅田铜多金属矿在其近几十年的找矿探矿史上,一直未取得重大的突破。本文通过对矿区从区域到矿床的地质特征进行细致的研究,认为杨梅田铜多金属矿属于典型的构造热液型脉状矿床,矿体的产出受地层岩性、断裂构造和热液控矿等控制因素的影响,为矿区的找矿探矿工作提供一定的指导和参考作用。
Yangmeitian copper polymetallic ore has not made major breakthroughs in its history of exploration and prospecting in recent decades. It is believed that Yangmeitian copper polymetallic ore is a typical tectonic hydrothermal vein deposit through a detailed study on the geological characteristics of the mining area from the area to the deposit. And the output of ore bodies is affected by controlling factors such as stratum lithology, fault structure and hydrothermal ore control, provide some guidance and reference for the exploration and prospecting work in the mining area.
引文
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