From plutons to magma chambers: Thermal constraints on the accumulation of eruptible silicic magma in the upper crust
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference56 articles.
1. The genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006
2. Thermal constraints on the emplacement rate of a large intrusive complex: the Manaslu Leucogranite, Nepal Himalaya;Annen;J. Petrol.,2006
3. Conditions for the growth of a long-lived shallow crustal magma chamber below Mount Pelee volcano (Martinique, Lesser Antilles Arc);Annen;J. Geophys. Res.,2008
4. On the origin of crystal-poor rhyolites: extracted from batholithic crystal mushes;Bachmann;J. Petrol.,2004
5. Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies;Bachmann;J. Volcanol. Geotherm. Res.,2006
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