摘要
讨论了山东莱州地区菱镁矿的地质特征及其成因,认为该区菱镁矿是经历了沉积成岩、变质作用和局部含镁热液交代而形成的。
Geological characteristics and genesis of magnesite deposits in Laizhou, Shandong province were discussed. It is believed that the magnesite deposits had been experienced sedimento-diagensis, metamorphism and magnesium-rich hydrothermal activities and lastly formed as sedimento-metamorphic magnesite deposits.
出处
《地质与勘探》
CAS
CSCD
北大核心
1997年第5期16-20,共5页
Geology and Exploration
关键词
菱镁矿矿床
地质特征
成因分析
粉子山群
magnesite deposit,geological characteristics,genesis analysis,Shandong
