玄武岩和金伯利岩深位捕虏体的研究可为岩石圈热演化和上地幔顶部的组成提供重要的信息。许多学者(Kushiro等,1976;Mercier,1979)认为火山岩中的捕虏体是被岩浆迅速带到地表的,在搬运过程中没有发生再平衡,基本保持了原来的面貌。因此对捕虏体适当的矿物组合使用地质温度计和地质压力计可以重建捕虏体被岩浆携带到地表这一进程期间下覆 The study of deep xenoliths in basalt and kimberlite can provide important information for the thermal evolution of the lithosphere and the composition of the top of the upper mantle. Many scholars (Kushiro et al., 1976; Mercier, 1979) think that the xenoliths in the volcanic rocks are rapidly brought to the surface by the magma and have not rebalanced during transportation and have basically maintained their original appearance. Therefore, a suitable combination of minerals for xenoliths can be reconstructed using geologic thermometers and geostresses to allow xenoliths to be submerged into the surface by magma