Syllabus ISM
Metamorphic Rocks/EPCC/LM6
Metaplate
Usgs low sulfide quartz gold deposit model
Chapter 8: Metamorphism and Metamorphic Rocks: New Rocks from Old.
1 Metamorphic Petrology Review Spring 2015. 2 Important Note Material from this review may appear on the final examination, in the same or somewhat altered.
Chapter 26: Metamorphic Reactions l If we treat isograds as reactions, we can: F Understand what physical variables might affect the location of a particular.
Metamorphic Rocks. Metamorphism and Metamorphic Rocks What is metamorphism? How do temperature and pressure change rocks? Are fluids important in metamorphism?
Metamorphic Facies: Reminder of principle metamorphic changes: 1/ Recrystallizationchanges in grain size responding to T & P changes. Coarsening of grains.
Metamorphic Reactions Reading: Winter Chapter 26.
Gibbs Phase Rule The number of variables which are required to describe the state of a system: p+f=c+2 f=c-p+2 –Where p=# of phases, c= # of components,
Chapter 26: Metamorphic Reactions If we treat isograds as reactions, we can: Understand what physical variables might affect the location of a particular.
