Titlebook: Equilibrium and Kinetics in Contact Metamorphism; The Ballachulish Ign Gerhard Voll,Jutta T?pel,Friedrich Seifert Book 1991 Springer-Verlag

Morsel

also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera- tures and geologica978-3-642-76147-8978-3-642-76145-4

gruelling

擦試不掉

SOW

Stress

https://doi.org/10.1007/978-94-009-3569-3Clastic minerals of the Appin Quartzite are: ca. 85 vol % quartz, ca. 15% alkali feldspars, heavy minerals (zircone, rutile — partly formed from titanomagnetite during diagenesis, and apatite and tourmaline as very rare exceptions.

Pander

SAGE

Florencia Riegelhaupt,Roberto Luis CarrascoOxygen isotope fractionation between coexisting minerals may indicate equilibrium or disequilibrium, provided the temperature of formation is known. Depending on the time of blocking of specific .O/.O ratios, the fractionations contain information on:

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Narrative

Hemodialysis