脉岩与热液脉状金矿化的时空伴生及其地质意义  

TEMPORAL-SPATIAL ASSOCIATION BETWEEN DYKE ROCK AND HYDROTHERMAL VEIN GOLD MINERALIZATION AND ITS IMPLICATION

作　　者：罗天明[1] 

机构地区：[1]冶金工业部天津地质研究院,天津300061

出　　处：《矿产与地质》1992年第2期118-125,共8页Mineral Resources and Geology

摘　　要：以我国东部吉黑、辽南及胶东等地区主要金矿床为例,从脉岩与热液金矿脉的空间、时间关系角度,探讨了脉岩与金矿化之间的成因关系。Based on the study of the relationship in space and time between dyke rock and hydrothermal gold vein in eastern China,such as Jilin Province,Heilongjiang Province,the south of Liaoning and the east of Shangdong Province,the genetic relationship between dyke rock and gold mineralization is dicussed in this paper.

关 键 词：金矿床 脉岩 时空关系 成因 

分 类 号：P618.510.1[天文地球—矿床学]