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
基金
Project supported by the National Natural Science Foundation of China
