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地幔岩是当前地质界正在积极开展研究的一个重要基础地质问题。它的研究有助于了解地球的组构和演化,查明基性、超基性岩及有关矿产的生成机制。二辉橄榄岩团块,通常是作为地幔岩残体进行研究的。可是一般该岩石团块多产在新生代、中生代一些碱性玄武岩的捕虏体中,而在我国新疆达拉布特华力西褶皱带,它却见于超基性岩体内。其发现和研究,将对探讨深部地质、了解铬矿成因和找矿,以及发展地幔岩岩石学和矿物学,将具
Mantle rocks are an important basic geological issue that the current geological community is actively carrying out research. Its research helps to understand the structure and evolution of the earth and to identify underlying, ultramafic rocks and related mineral formation mechanisms. Litter gneiss, often studied as mantle rock remnants. However, in general, the rock mass is prolific in the Xenoliths of some basalts of the Mesozoic and Mesozoic Era, whereas in the Valsalva fold belt of the Dalbute of Xinjiang Uygur Autonomous Region, it is found in ultramafic rocks. Its discoveries and studies will provide insight into deep geology, understanding the causes and prospecting of chromite, and the development of mantle rock petrology and mineralogy,