摘要
遂安石的微结构主要表现为位错、相畴及调置结构,这些结构反映了矿床变质作用的热历史,这一过程表现为升温及升温后的退火作用。
Main microstructure of suanite are dislocation, domain and modulation.These structure are feedback of the heat history of the metamorphism about the doposit.The process suffered raising tcmperature and afterward the annealing.
出处
《世界地质》
CAS
CSCD
1997年第4期27-30,共4页
World Geology