Geothermobarometry Partioning of Fe, Mg with Temperature: The Garnet-Biotite Geothermometer Fe, Mg have similar ionic radii, therefore volume change small The Garnet ...
Geothermobarometry How do we know P and T? Geothermobarometry Need min. at equilibrium Good barometer rxn vs. good thermometer rxn Which has large DV and which has ...
Yet they are not accurate, because they do not hit the bulls-eye. b. ... but they are accurate, because the average of the shots is near the bulls-eye. c. ...
Thermodynamics Begin with a brief review of Chapter 5 Natural systems tend toward states of minimum energy Figure 27.13. P-T pseudosection calculated by THERMOCALC ...
P-T-t Paths and Their Significance Metamorphic Field Gradient Trend of Thermal Maxima Across Metamorphic Facies Clockwise P-T-t Path P-T-t Path Reflecting Crustal ...
Consider a plane of unit area oriented at an angle Q to the principal stress ... Plastic strength of rocks Continuum Mechanics: Brittle Failure Continuum ...
0 deg C for surface; 1300 deg C for base of lithosphere (100 km before thickening) ... Delamination of thickened lithosphere * Result of convective mantle flow ...
T-X phase diagram of the system albite-orthoclase at ... of several determined univariant reactions in the CaO-MgO-Al2O3-SiO2-H2O-(Na2O) system ( C(N)MASH ...
... petrogenetic grid for metamorphosed mafic rocks showing the location of several determined univariant reactions in the CaO-MgO-Al2O3-SiO2-H2O-(Na2O) system ...
More Ca-rich plagioclases become progressively unstable as T lowered ... pressure-temperature-time paths based on a crustal thickening heat-flow model. ...
... between olivine and melt is strongly dependent on the MgO content of the olivine ... kh is a proportionality constant called the Henry's law constant ...