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- W3202380304 abstract "发生在会聚边缘的构造和岩浆过程对于地壳和地幔的演化是重要的。会聚边缘是岩基形成和许多成矿作用发生的场所,并在那儿形成陆壳和地壳受到分馏及残余体被再循环回到地幔。因此,越来越多的意义深远的文献专注于陆缘(安第斯型)和洋内弧系的古代和现代火成产物。" @default.
- W3202380304 created "2021-10-11" @default.
- W3202380304 creator A5004676538 @default.
- W3202380304 date "1993-10-31" @default.
- W3202380304 modified "2023-09-23" @default.
- W3202380304 title "俯冲带幼年期:来自始新世伊豆-小笠原-马里亚纳弧和侏罗纪加利福尼亚弧的实例" @default.
- W3202380304 hasPublicationYear "1993" @default.
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