Energy-Constrained Open-System Magmatic Processes II: Application of Energy-Constrained Assimilation–Fractional Crystallization (EC-AFC) Model to Magmatic Systems

By W. Bohrson, F. Spera. 2001

282 citations recorded by the source corpus.

Subfields: Artificial Intelligence, Geophysics

View Paper: https://www.semanticscholar.org/paper/6b92e33bfbc5819312f7e30f454387b443ae6149

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In Artificial Intelligence

1. O. Bachmann
2. G. Bergantz
3. F. Spera

In Geophysics

1. O. Bachmann
2. G. Bergantz
3. F. Spera

Citations in the corpus

• Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies (2006, methodology): “Using the following values (DTmush of 50 8C, DTmafic of 100 8C, vc of 90%, vm of 0%, Lmush of 2.7 10(5) J/kg, Lmafic of 4 10(5) J/kg, Cpmush of 1370 J/kg K and Cpmafic of 1484 J/kg K; Bohrson and Spera, 2001), mmush / mmafic is ~7.”
• Energy-constrained open-system magmatic processes I : General model and energy-constrained assimilation and fractional crystallization (EC-AFC) formulation (2001, methodology): “Energy-Constrained Open-System Magmatic Processes I: General Model and EnergyConstrained Assimilation and Fractional Crystallization (EC-AFC) Formulation”