12.480 Thermodynamics for Geoscientists, Spring 2004

12.480 Thermodynamics for Geoscientists, Spring 2004

Principles of thermodynamics are used to infer the physical conditions of formation and modification of igneous and metamorphic rocks. Includes phase equilibria of homogeneous and heterogeneous systems and thermodynamic modelling of non-ideal crystalline solutions. Surveys the processes that lead to...

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Détails bibliographiques
Auteur principal: Grove, Timothy L.
Autres auteurs: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Learning Object
Langue:en-US
Publié: 2004
Sujets:
tectonic environments
crust
mantle
Ideal Solutions
Non-ideal Solutions
Pyroxene Thermometry
Plagioclase Feldspars Solution Models
Alkali Feldspars Solution Models
Multi-site Mineral Solutions
Homogeneous Equilibria
Quad
Spinels
Rhombohedral Oxides
T-ƒO2 Relations
Heterogeneous Equilibria
Multi-Component Systems
Liquidus Diagrams
Schreinemaker's Analysis
Composition Space
Gibbs Method
Silicate Melts
Mixed Volatile Equilibria P-T-XCO2-XH2O
thermodynamic models
thermodynamics
Accès en ligne:http://hdl.handle.net/1721.1/41054

Internet

http://hdl.handle.net/1721.1/41054

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