摘要
玲珑断裂是一条成矿前即已存在的重要导矿断裂,早期表现为右行走滑,晚期表现为左行走滑,对西山的成矿起到了重要作用。受玲珑断裂影响,矿脉在水平方向上呈等间距分布,在纵向上矿体主要位于距玲珑断裂西100~150 m和600~800 m的范围内,并且控制了矿体NE向侧伏。
Linglong fault is an important ore-conducting fructure which has been existing before mineralizing.Its early and late characteristics are right-parallel and left-parallel strike-slip fault respectively,which plays an im-portant role in mineralization of Xishan mountain.Affected by Linglong fault,the ore vein is equal interval horizon-tally and located within the scope of 100~150 m and 600~800 m longitudinally to the west of Linglong fault,which has controlled the NE-extending of ore body.
出处
《黄金科学技术》
2010年第2期35-39,共5页
Gold Science and Technology
关键词
地质特征
找矿意义
玲珑断裂
山东省
Geological characteristics
Significance of ore prospecting
Linglong fault
Shandong Province
