摘要
辽吉裂谷在拱张、裂陷、下沉、上升和挤压消亡过程中,沉积了巨厚的碎屑沉积物,并发生多次强烈的构造活动、岩浆活动、变质变形作用及深部的壳幔作用。通过对辽吉裂谷的演化和成矿模式、裂谷内铅锌矿床的成因类型和其地球化学行为的分析,认为裂谷作用为铅锌矿形成提供了丰富的矿源、富集成矿的场所和有效的热能、裂谷演化中物理化学条件的改变和岩浆活动也使得成矿物质进一步富集成矿。
Globally, many Pb-Zn ore are hosted in rifts. Especially the mega Pb-Zn ore deposit-Jiande Pb- Zn ore deposit of Korea is occurred in Liaoji rift. It is obvious that the relation of rift and mineral resources is intimate. In the poeess of arch-stretching, rifting ,sinking, uplifting and compression, disappearance of the rift, mega-thick elastic sediments and many violent tectonic, magmatism,metamorphism and deformation, the deep crust-mantle interaction took place. The evolution of Liaoji rift, the metallogenic model, the genetic types of Pb-Zn ore deposits in the rift and its geochemical behavior is analyzed. The authors think： that the rift provide the abundant ore source, the location of enrichment and mineralization and the effectual thermal energy for ore formation, the change of physical-chemical condition of the rift evolution and mag- matism, make the minerogenic matter more enrichment and mineralization.
出处
《地质找矿论丛》
CAS
CSCD
2006年第1期19-22,27,共5页
Contributions to Geology and Mineral Resources Research
基金
中国地质调查局"华北地台成矿规律和找矿方向综合研究项目"(编号:200110200038)资助
关键词
裂谷演化
铅锌矿
成因类型
成矿模式
成矿作用
rift evolution
Pb-Zn ore deposit
genetic type
metallogenic model
mineralizaton
