Premium
On equilibrium in non‐hydrostatic metamorphic systems
Author(s) -
Powell R.,
Evans K. A.,
Green E. C. R.,
White R. W.
Publication year - 2018
Publication title -
journal of metamorphic geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.639
H-Index - 114
eISSN - 1525-1314
pISSN - 0263-4929
DOI - 10.1111/jmg.12298
Subject(s) - metamorphic rock , metamorphism , geology , mineral , hydrostatic equilibrium , simple (philosophy) , realization (probability) , crust , geochemistry , mathematics , chemistry , statistics , physics , epistemology , quantum mechanics , philosophy , organic chemistry
Abstract Metamorphic geology has accumulated a huge body of observation on mineral assemblages that reveal strong patterns in occurrence, summarized, for example, in the idea of metamorphic facies. On the realization that such patterns needed a simple explanation, there has been considerable a posteriori success from adopting the idea that equilibrium thermodynamics can be used on mineral assemblages to make sense of the patterns in terms of, for example, the pressure and temperature of formation of mineral assemblages. In doing so, a particularly simple implicit assumption is made, that mineral assemblages operate essentially hydrostatically. Structural geologists have studied the same rocks for different ends, but, remarkably, the phenomena they are interested in depend on non‐hydrostatic stress. We look at the effect of such behaviour on mineral equilibria. With adoption of some plausible assumptions about how metamorphism in the crust works, the consequence of minerals being non‐hydrostatically stressed is commonly second order in equilibrium calculations.