THE NEWEST TESTIMONY OF MAGMATIC ORIGIN OF SPILITE  

作　　者：夏林圻 夏祖春 

机构地区：[1]Xi'an Research Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences. Xi'an 710054, PRC

出　　处：《Chinese Science Bulletin》1990年第3期217-222,共6页

基　　金：Project supported by the National Natural Science Foundation of China

摘　　要：The genesis of spilite-keratophyric volcanic rock assemblages being the important part of submarine volcanic rocks has long been in contention, the focus of which is the origin of sodium. Basing on the discoveries of albite with disorder-transition structure in spilite-keratophyre and the primary sodic magmatic inclusions in quartz phenocrysts

关 键 词：SPILITE CLINOPYROXENE MAGMATIC inclusion. 

分 类 号：N[自然科学总论]