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Geoscience > Geology > Igneous and Metamorphic Petrology > PTt Relationships
5 matchesResults 1 - 5 of 5 matches
Calculating Compositional Variation and Common Substitutions for Igneous and Metamorphic Minerals part of Petrology:Teaching Examples
Dave Mogk, Montana State University-Bozeman
This problem set uses Excel spreadsheets to calculate mineral formulae from analytical data (typically from the electron microprobe) using a variety of formulations that assume numerous variations of crystal ...
Resource Type: Activities: Activities:Problem Set
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:Igneous Processes, Metamorphic Processes, Geoscience:Geology:Mineralogy:Phase Equilibria/Thermodynamics, Geoscience:Geology:Igneous and Metamorphic Petrology:Geochemistry, PTt Relationships, Thermodynamics and Phase Equilibria, Geoscience:Geology:Geochemistry:Phase Equilibria/Thermodynamics
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T-X Phase Diagrams part of Petrology:Teaching Examples
Dexter Perkins, University of North Dakota-Main Campus
This is a 15 page tutorial and problem set designed to get students familiar with T-X diagrams, their implications, and uses.
Resource Type: Activities: Activities:Classroom Activity, Lab Activity, Problem Set
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:PTt Relationships, Thermodynamics and Phase Equilibria, Metamorphic Processes, Geoscience:Geology:Geochemistry:Phase Equilibria/Thermodynamics
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Schreinemakers Analysis - Problem #3: Analysis of an Invariant Point part of Petrology:Teaching Examples
Dexter Perkins, University of North Dakota-Main Campus
This is a challenging Schreinemakers analysis problem.
Resource Type: Activities: Activities:Problem Set, Classroom Activity
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:Thermodynamics and Phase Equilibria, PTt Relationships
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Schreinemakers Analysis - Problem #4 part of Petrology:Teaching Examples
Dexter Perkins, University of North Dakota-Main Campus
This is a straightforward Schreinemakers analysis involving two invariant points.
Resource Type: Activities: Activities:Classroom Activity, Problem Set
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:Thermodynamics and Phase Equilibria, PTt Relationships, Geoscience:Geology:Geochemistry:Phase Equilibria/Thermodynamics
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Mass Balance and Mineral Reactions part of Petrology:Teaching Examples
Dexter Perkins, University of North Dakota-Main Campus
This is a short exercise to make sure that students understand mass balance and how the different starting assemblages may lead to different results after metamorphism. It is quick but not trivial.
Resource Type: Activities: Activities:Classroom Activity, Problem Set
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:Metamorphic Processes, PTt Relationships, Thermodynamics and Phase Equilibria
Activity Review: Peer Reviewed as Exemplary
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