山东煤炭科技
山東煤炭科技
산동매탄과기
Shandong Coal Science and Technology
2015年
8期
151-152
,共2页
公婆泉二区%铜矿%矿石特征%成因
公婆泉二區%銅礦%礦石特徵%成因
공파천이구%동광%광석특정%성인
the second district of Gongpoquan%copper%the characteristics of copper ore%genesis
公婆泉二区铜矿床位于马鬃山早古生代岩浆弧单元南部，与公婆泉铜矿比邻，该文介绍了铜矿石的特征，大致划分了矿区主要矿脉的矿石类型以及对矿床的成因进行初步探讨，该区矿床应为热液成因。
公婆泉二區銅礦床位于馬鬃山早古生代巖漿弧單元南部，與公婆泉銅礦比鄰，該文介紹瞭銅礦石的特徵，大緻劃分瞭礦區主要礦脈的礦石類型以及對礦床的成因進行初步探討，該區礦床應為熱液成因。
공파천이구동광상위우마종산조고생대암장호단원남부，여공파천동광비린，해문개소료동광석적특정，대치화분료광구주요광맥적광석류형이급대광상적성인진행초보탐토，해구광상응위열액성인。
The second district of Gongpoquan copper is located in the early Paleozoic magmatic arc unit from the south of Mazong mountain, nearly to the Gongpoquan copper. It introduces the characteristics of copper ore, divides the ore types of the main vein in this mine lot and preliminarily discusses the genesis of ore deposit, which is hydrothermal origin.
