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东昆仑造山带三叠纪花岗岩类和流纹岩类的成因:洋壳到陆壳的转化 学位论文
, 北京: 中国科学院大学, 2017
Authors:  邵凤丽
Adobe PDF(8170Kb)  |  Favorite  |  View/Download:412/3  |  Submit date:2017/05/31
东昆仑造山带  同碰撞花岗岩类  洋壳熔融  大陆地壳生长  过碱性流纹岩