Argon isotopic composition of rock and ore formed during the orogenic process in Altay, Xinjiang, shows that the building of the Altay orogenic were related to crust-mantle interaction, and that mantle degassing was obviously existed.
通过对新疆阿尔泰造山过程中形成的岩石、矿石样品氩同位素组成的研究 ,认为阿尔泰造山带的形成与壳幔相互作用有关 ,造山过程中的地幔脱气现象是存在的。
参考来源 - 阿尔泰造山带岩石和矿石的氩同位素研究·2,447,543篇论文数据,部分数据来源于NoteExpress
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