摘要
从地球物理学、实验岩石学、岩石学和地球化学几个方面论述了青藏高原已具备壳内发生大规模部分熔融的物理环境及物质基础；
From several aspects,such as geophysics,experimental petrology,petrology and geochemistry,this paper states that there are physical conditions and material basis of melting in wide scale in Tibetan Plateau.Then the relationship between intracrustal partial melting and thickening of Tibetan Plateau as well as three possible thickening models are discussed.
出处
《地质科技情报》
CAS
CSCD
北大核心
1999年第1期24-28,共5页
Geological Science and Technology Information
基金
国家自然科学基金
地矿部行业基金
博士点基金
关键词
部分熔融作用
底浸作用
青藏高原
地壳加厚
partial melting,underplating,anomalously thickening crust,Tibetan Plateau
