【摘 要】
：
The source rock from which the sillimanite gneisses derive mainly was the biotite plagioclase gneiss in the Larsemann Hills.It is the deformation-metamorphism process under special pressure and temper
【出 处】
：
Chinese Journal of Polar Science
论文部分内容阅读
The source rock from which the sillimanite gneisses derive mainly was the biotite plagioclase gneiss in the Larsemann Hills.It is the deformation-metamorphism process under special pressure and temperature condition,not the original rock compositions,t
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