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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Manylion Llyfryddiaeth
Prif Awdur:	Grove, Timothy L.
Awduron Eraill:	Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Fformat:	Learning Object
Iaith:	en-US
Cyhoeddwyd:	2004
Pynciau:	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
Mynediad Ar-lein:	http://hdl.handle.net/1721.1/41054

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

12.480 Thermodynamics for Geoscientists, Spring 2004

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