前进变质作用
The middle Proterozoic crystalline schist series in the Panzhihua-Xichang region has undergone progressive regional metamorphism.
攀西中元古结晶片岩系遭受了前进区域变质作用。
The time of intrusion and uplift of granite located in the thermal center lag that of domal progressive metamorphism, there is no origin connection between metamorphism and igneous intrusion.
热中心花岗岩的侵位和上隆滞后于穹状递增变质作用,二者在成因上无直接的联系。
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