摘要
本文从构造地球化学角度研究了包裹体的形态特征、均一温度、氢、氧同位素及包裹体气液成分的变化规律与构造形变的关系，认识到可从包裹体研究认识构造岩流体的演变规律，从而更进一步地认识构造活动中的地球化学作用。
This paper deals with the relationship between the characteristics of inclusions, homogenization temperatures, H and O isotopic composition of the inclusions, variation of gaseous and liquid constituents in the inclusions on one hand and tectonic deformation on the other hand. This study sheds light on the evolution of tectonite fiuid as well as the geochemical processes during tectonic deformation.
出处
《地质地球化学》
CAS
CSCD
北大核心
1997年第1期37-41,共5页
Geology-Geochemistry
基金
国家自然科学基金
