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地壳深部的变质流体可能也是呈幕式活动并产生幕式的构造运动。
The metamorphic fluid activity in the deep parts of crust can be in episodic manner and produce episodic tectonic movements.
副矿物和退变质流体是控制退变质过程中微量元素行为的主要因素。
Accessory minerals and retrograde fluids are main factors controlling the trace elemental behavior during retrograde metamorphism.
盆山转换时期所形成的变质流体为多相盐水流体，形成于变形的初期。
The studies indicate that the fluid formed during the basin mountain transition is metamorphic fluid with multi phase salt water formed in the initial stage of deformation.
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