摘要
八道金矿为延吉中生代火山岩型金矿中较为典型的矿床之一。其矿床成因,除与火山作用有关之外直接受构造的控制,而火山作用本身又与区域深大断裂有关。本文着重讨论了矿区火山岩与朝阳河断裂的关系及构造控矿模式。
The Badao gold deposit is a typical Mesozoic volcanic rock-hosting gold deposit. The genesis of the deposit was connected with vocanism and directly controlled by structure. The volcanism is connected with the regional deep fault belt. This paper emphatically studies the connection with local volcanism and the Chaoyang River fault, and discusses the structural ore-controlling model.
出处
《地质地球化学》
CSCD
北大核心
1998年第2期22-28,共7页
Geology-Geochemistry
关键词
金矿床
矿床构造
控矿模式
构造应力
volcanic gold deposit
deep fault belt
tenso-shear fault
structural stress
structural ore-controlling model