摘要
叠加-重熔型花岗岩“并列成岩成矿系列片段”模式,是基于地壳深部半开放性多岩浆房平行演化的认识建立的。它既反映了单岩浆房花岗岩浆“单向式”演化的规律性和形成相对完整成岩成矿系列的可能性,同时也代表了南岭多旋回叠加-重熔型花岗岩类演化的总趋势。
The establishment of the parallel petrogeno-mineralization series model for superimposed-remolten granites is based on the information on the parallel evolution of semi-open, multiple magma chambers in the interior of the crust. This model reflects not only the regularity gover-ning the 'single-direction' evolution of granitic magma from a single magma chamber but also the possibility of forming a relatively complete petrogeno-mineralization series. The model also characterizes the general trend of the evolution of multicyclic, superimposed-remolten granites in the Nanling region.
出处
《地球化学》
CAS
CSCD
北大核心
1989年第1期43-51,共9页
Geochimica
