摘要
本文从矿床的描述模式、分布规律、成矿物质来源和成矿模式等4个方面探讨了西秦岭褶皱系层控矿床的共生规律,指出该区层控矿床的共生规律与西秦岭褶皱系地槽发展特点密切相关,其褶皱系的次级活动构造单元之间分界深断裂带的活动规律则是控制该区层控矿床的最基本因素.
The paragenetic regularity of the stratabound mineral deposits in the western Qinling fold system is discussed in the light of metallization types, distribution features, source materials and metallogenetic pattern. It has to be poind out that the paragenetic regularity of the deposits in this area is closely related to the development of the geosyncline in the western Qinling fold system, and the mobile regularity of the bounded deep fracture zone between the secondary mobil tectonic units is the most essential factor for ore controlling of the stratabound deposits in this area.
出处
《地质与勘探》
CAS
CSCD
北大核心
1991年第4期3-13,共11页
Geology and Exploration
