Igneous rock associations 5. oceanic island volcanism II: mantle processes.(Series)

From: Geoscience Canada | Date: June 1, 2005| Author: Dostal, Jaroslav; Greenough, John D.; Mallory-Greenough, Leanne M. | Copyright information

SUMMARY

Oceanic island basalts (OIBs) have been central to understanding evolution of the Earth and mantle because their isolated positions in ocean basins limit the potential for magma contamination by continental crust. Melting processes (e.g., percentage melting) affect OIB chemistry but isotopic and trace-element ratios provide information on mantle-source compositions. They indicate that OIB mantle sources represent mixtures between mid-ocean ridge basalt (MORB) man...

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