摘要
作者于1979年开始提出多因复成矿床概念的主旨，是为了阐明从时空四维并重的角度来认识与研究成矿的重要性。作者认为：多因复成矿床以“五多”为特点。其中多成矿大地构造演化阶段是产生其他“四多”(多成矿类型、多控矿因素、多成矿作用和多成矿物质来源)的关键而属于主导地位的“一多”。由于多因复成矿床概念体现了历史—动力综合大地构造学所强调的四维思维，即把时间与三维空间兼顾的思维方法，所以这类矿床的“五多”特点中，以多成矿大地构造演化阶段这“一多”为最主要。
The conception of polygenetic compound deposit, mainly from an equal－ stressed angle of time－ space four dimensions, is used to interpret and discuss metallogenic problems.Polygenetic compound deposit is characterized by “ five many” .Among them the many metallo－ geotectonic evolution stages is the predominant one,which gives rise to the other“ four many” (many metallogenic types,many ore－ controlling factors,many ore－ forming processes and many ore－ forming materials sources).Because the conception of polygenetic compound deposit embodies four－ dimesion characteristics emphasized by historical－ dynamic integrative geotectonic system,namely giving consideration to time and three dimension space,among the above“ five many” features of this type of deposit,many metallogenetic evolution stages is the most principal.
出处
《大地构造与成矿学》
EI
CAS
CSCD
2000年第3期199-201,共3页
Geotectonica et Metallogenia
基金
中国科学院"九五"重点项目!"壳体大地构造的演化与运动及其机制研究"(项目编号:KZ952-J1-007)资助.
关键词
多因复成矿床
四维思维方法
大地构造演化
成矿
Polygenetic compound deposit
time－ space four dimension method
geotectonic evolution stage
