摘要
初步讨论了华北地区燕山期区域变质作用与内生成矿作用的关系。指出华北地区众多内生金属矿床产于绿片岩相岩石组合中,其中包括太古宙岩石的退变质、沉积盖层和中生代火山-侵入杂岩的进变质岩石。因此,这些矿床的形成与燕山期区域变质作用及其相应的韧性-韧脆性变形作用密切相关。
During Yanshanian (Jura-Cretaceous) tectonic event of North China, both of the Archean basement and sedimentary cover were involved in the regional metamorphism due to thrusting and magmatism. Many ore deposits in North China occurred in green-schist facies rock assemblage. It was suggested that the ore-bearing green-schist facies rock assemblages were mainly formed by Yanshanian regressive metamorphism of Archean rocks and prograde metamorphism of sedimentary cover rocks. Therefore, the origin of many ore deposits in North China was caused by the Yanshanian regional metamorphism and related ductile deformation.
出处
《北京地质》
2005年第3期29-33,共5页
Beijing Geology
基金
国家自然科学基金项目(No.40376013
40104003)
中国博士后科学基金
中国科学院王宽诚博士后奖励基金资助.