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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Language: | en-US |
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2004
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Online Access: | http://hdl.handle.net/1721.1/41054 |
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author | Grove, Timothy L. |
author_facet | Grove, Timothy L. |
author_sort | Grove, Timothy L. |
collection | MIT |
description | 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 the formation of metamorphic and igneous rocks in the major tectonic environments in the Earth's crust and mantle. |
first_indexed | 2024-09-23T16:03:58Z |
id | mit-1721.1/41054 |
institution | Massachusetts Institute of Technology |
language | en-US |
last_indexed | 2024-09-23T16:03:58Z |
publishDate | 2004 |
record_format | dspace |
spelling | mit-1721.1/410542019-09-12T10:15:41Z 12.480 Thermodynamics for Geoscientists, Spring 2004 Thermodynamics for Geoscientists Grove, Timothy L. 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 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 the formation of metamorphic and igneous rocks in the major tectonic environments in the Earth's crust and mantle. 2004-06 12.480-Spring2004 local: 12.480 local: IMSCP-MD5-749afb2e33e738e61689b14a019c1ecc http://hdl.handle.net/1721.1/41054 en-US Usage Restrictions: This site (c) Massachusetts Institute of Technology 2003. Content within individual courses is (c) by the individual authors unless otherwise noted. The Massachusetts Institute of Technology is providing this Work (as defined below) under the terms of this Creative Commons public license ("CCPL" or "license"). The Work is protected by copyright and/or other applicable law. Any use of the work other than as authorized under this license is prohibited. By exercising any of the rights to the Work provided here, You (as defined below) accept and agree to be bound by the terms of this license. The Licensor, the Massachusetts Institute of Technology, grants You the rights contained here in consideration of Your acceptance of such terms and conditions. text/html Spring 2004 |
spellingShingle | 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 Grove, Timothy L. 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title | 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title_full | 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title_fullStr | 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title_full_unstemmed | 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title_short | 12.480 Thermodynamics for Geoscientists, Spring 2004 |
title_sort | 12 480 thermodynamics for geoscientists spring 2004 |
topic | 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 |
url | http://hdl.handle.net/1721.1/41054 |
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