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.
根据熔浆-矿物平衡热力学，岩浆被认为起源于榴辉岩相条件下俯冲板片的部分熔融。
Based on the melt-mineral equilibrium thermodynamics, it is believed that the adakitic magma originated by partial .
当你口渴的时候，可以饮用普通的、清凉的、无卡路里的水，同时每天摄入一定量的复合维生素剂来维持身体必须维生素和矿物质的平衡。
Drink plain, refreshing, calorie-free water when you\\\'re thirsty—and take a multivitamin daily to make sure you get balanced levels of the essential vitamins and minerals.
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