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1.- Evidence from a crystal-poor, zoned (rhyolite-andesite) pyroclastic deposit from Volcan Tepetiltic, western Mexico for rapid generation of silicic melt by partial melting of granitoid and not by segregation from a long-lived crystal-rich mush
American Geophysical Union; Washington, DC; USA; United States, 2007
AGU 2007 fall meeting
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