摘要
四川省代隆金矿位于壤塘金矿带内,该带总体呈北西西向,由一系列断层及褶皱组成,并伴有不同岩性的岩浆岩产出。区内构造整体呈北西西向,但也发育东西向及北东向次级断裂。区内金矿体主要富集在花岗斑岩与板岩之间的断裂破碎带内,在北西西向与东西向构造结合部位、北西西向构造产状变化部位,为下一步找矿有利部位。
The Dailong Au deposit is located in the Zamtang Au ore zone which is composed of a series of NWW-trending faults and folds as well as magmatic rocks.The Au deposit is confined to rupture zone between granite porphyry and slate.Intersection of NWW-trending structure with latitudinal structure is favorable for Au ore-formation.
出处
《四川地质学报》
2010年第3期298-301,共4页
Acta Geologica Sichuan
关键词
金矿
构造控矿
找矿方向
四川代隆
Au deposit
ore control structure
range of reconnaissance
Dailong Sichuan
