The P-T conditions the rocks experienced after peak metamorphism are deduced from the mineral equilibria and the microthermometry of the fluid inclusions.
根据矿物平衡和流体包裹体资料推断了峰期变质后岩石经历的P -T条件。
The P-T conditions the rocks experienced after peak metamorphism are deduced from the mineral equilibria and the microthermometry of the fluid inclusions.
根据矿物平衡和流体包裹体资料推断了峰期变质后岩石经历的P -T条件。
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