摘要
综述了板块构造、大地构造单元、区域构造、深大断裂以及地球深部热点与斑岩铜矿床形成关系的研究成果,系统介绍了斑岩铜矿床蚀变矿化分带特征、蚀变矿化物理化学条件、蚀变矿化的热力学研究、斑岩铜矿床中脉体的产状和分布特征以及成因观点,总结了斑岩铜矿床成矿物质来源与矿床成因模式,最后指出了斑岩铜矿床将来应该注意的研究方向。
The main achievements of the genetic relationships between porphyry copper depositsand plate tectonics, tectonic unit,regional structure,long and deep regional fracture andhot point in the mantle are summarized.The most important characteristics of zoning ofalteration and mineralization and the primary features of distribtition and dips of veins inporphyry copper deposits as well as genetic views for the veins are synthesized.The signif-icant investigations about physico-chemical coditions of rock-forming and ore-forming pro-cesses,the sources of ore-forming matter, the major genetic patterns for the deposits andsome important aspects which should be studied in detail by complex sciences are show inthis article.
出处
《地球科学进展》
CAS
CSCD
1995年第1期40-46,共7页
Advances in Earth Science
基金
国家自然科学基金
关键词
斑岩铜矿床
蚀变
矿化
成因模式
脉体
铜矿床
Porphyry copper deposit, Alteration , Mineralization,Vein,Genetic pat-tern.