A Thermodynamic Model of Adiabatic Melting of the Mantle
<p>Mid-ocean ridge basalts (MORB) are mixtures of melts produced over a range of pressure and temperature in a nearly adiabatic open system undergoing changes in composition as melting proceeds. Interpretation of the compositional variations observed in MORB and their correlation with geophys...
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| Format: | Others |
| Language: | en |
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1997
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| Online Access: | https://thesis.library.caltech.edu/4607/1/Asimow_pd_1997.pdf Asimow, Paul David (1997) A Thermodynamic Model of Adiabatic Melting of the Mantle. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/93RY-AN70. https://resolver.caltech.edu/CaltechETD:etd-11202003-144820 <https://resolver.caltech.edu/CaltechETD:etd-11202003-144820> |
Internet
https://thesis.library.caltech.edu/4607/1/Asimow_pd_1997.pdfAsimow, Paul David (1997) A Thermodynamic Model of Adiabatic Melting of the Mantle. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/93RY-AN70. https://resolver.caltech.edu/CaltechETD:etd-11202003-144820 <https://resolver.caltech.edu/CaltechETD:etd-11202003-144820>