地洼区的过渡间成矿──以广西某些多金属矿床为例  

Transitive Mineralization of Diwa Region-Taking Some of Metalliferous Deposits in Guangxi as Examples

作　　者：陈勤五 

机构地区：[1]广西地质矿产局

出　　处：《地质与勘探》1994年第6期23-26,34,共5页Geology and Exploration

摘　　要：按地洼成矿理论，着重研究了“地洼区的过渡间成矿”，即过渡层（岩性）成矿、过渡带成矿和地洼阶段过渡期成矿相结合的“三位一体”的大地构造成矿控矿的基本模式。并以广西某些多金属矿床为例，对其基本特征进行阐述。The transitive metallogeny of Diwa region″,namely,″three in one″tectonic metallogenic and ore-control model composedof transitive stratum(lithology)mineralization,transitive belt mineralization and Diwa stage transitive epoch mineralization is em-phasized,Its basic features are expounded by the examples of metalliferous deposits in Guangxi.

关 键 词：地洼 过渡带 成矿作用 多金属矿床 

分 类 号：P618.205[天文地球—矿床学]