摘要
随着岩浆体系结晶机理研究的不断深入,火山岩和侵入岩岩浆动力学理论已经进入到模型建立阶段。本文试图通过对安徽沙溪斑岩体进行实例研究,先求出斜长石斑晶的存储时间,再算得晶体成核速率和生长速率。
With the increasing deepening of the study on crystallization mechanism of the magmatic system, the magmatic kinetic theory of volcanic and intrusive rocks has entered the stage of establishing a model. Through the study of the example of Shaxi porphyry body in Anhui Province, the authors first figured out the storage time of plagioclase phenocrysts, then calculated the nucleation rate and growth rate of the crystals and , on such a basis, established the thermal model for cooling of the hypabyssal magmatic system
出处
《岩石矿物学杂志》
CAS
CSCD
北大核心
1997年第4期303-313,共11页
Acta Petrologica et Mineralogica
基金
国家自然科学基金
中国科学院专项基金
关键词
浅成岩浆
热模型
成核速率
生长速率
结晶机理
: hypabyssal magma
thermal model
grainsize statistics
nucleation rate
growth rate.