Petrology and geochemistry of altered ocenaic crust of ODP Hole 140-504B
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Altered basalt dikes from Hole 504B were partially melted at 1150°C and 1180°C to determine the composition of the first melts as oceanic Layer 2C is assimilated by a magma...
将取自504B钻孔（Hole 504B）的蚀变玄武岩岩脉分别在1150℃与1180℃条件下进行部分熔融实验，以明确当大洋2C层被岩浆同化时所产生的初始熔体的成分……
