摘要
在系统回顾地幔岩包体的研究简史及研究现状的基础上,对我国地幔岩包体今后的研究对策进行了探讨。认为我国地幔岩包体今后的研究工作应重视地幔岩包体形成演化过程中压力(p)、温度(T)、环境(E)和时代(t)的综合制约作用,定量模拟地幔岩包体的形成过程,最终建立地幔岩包体形成演化的pTEt模式。
On the basis of reviewing the research simple history and present situation, the present paper will approach the countermeasure for the research of the Chinese mantle xenoliths. We must emphasize the research of the systematical constraint of pressure ( p )、temperature ( T )、environment ( E ) and time ( t ) in the formation and evolution of mantle xenoliths, and model the process of formation quantitatively. At the last, we have established the pTEt model of the formation and evolution of mantle xenoliths.
出处
《世界地质》
CAS
CSCD
1998年第1期1-7,共7页
World Geology