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  2. Metamorphic series - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_series

    However, Buchan facies series plot along line 3 and Barrovian at somewhat higher pressure and with the appearance of kyanite. The facies series have connections to plate tectonics. Facies series 1 is typical of contact metamorphism, but also found in regional metamorphosed rocks. Facies series 2 correlates with volcanic arc environments, and so ...

  3. Metamorphic facies - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_facies

    A metamorphic facies is a set of mineral assemblages in metamorphic rocks formed under similar pressures and temperatures. [1] The assemblage is typical of what is formed in conditions corresponding to an area on the two dimensional graph of temperature vs. pressure (See diagram in Figure 1). [ 1 ]

  4. Compatibility diagram - Wikipedia

    en.wikipedia.org/wiki/Compatibility_diagram

    In metamorphic geology, a compatibility diagram shows how the mineral assemblage of a metamorphic rock in thermodynamic equilibrium varies with composition at a fixed temperature and pressure. Compatibility diagrams provide an excellent way to analyze how variations in the rock's composition affect the mineral paragenesis that develops in a ...

  5. Metamorphic zone - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_zone

    Often only part of the series can be found. Another metamorphic facies series is the Buchan series, that sees a fast increase in temperature but a relatively small increase in pressure. Characteristic minerals include andalusite, biotite and cordierite. The metamorphic prograde sequence of the Buchan zone series is:

  6. Petrogenetic grid - Wikipedia

    en.wikipedia.org/wiki/Petrogenetic_grid

    Figure 1 is an example of a complex petrogenetic grid for metamorphosed pelitic rocks. It shows most of the important reactions that govern the development of aluminous mineral assemblages from the prehnite-pumpellyite facies to the granulite facies , as well as the blueschist facies and eclogite facies at higher pressures and the contact ...

  7. Metamorphism - Wikipedia

    en.wikipedia.org/wiki/Metamorphism

    The facies are named after the metamorphic rock formed under those facies conditions from basalt. [79] The particular mineral assemblage is somewhat dependent on the composition of that protolith, so that (for example) the amphibolite facies of a marble will not be identical with the amphibolite facies of a pellite. However, the facies are ...

  8. File:Metamorphic facies EN.svg - Wikipedia

    en.wikipedia.org/wiki/File:Metamorphic_facies_EN.svg

    English: Diagram for metamorphic facies in the Earth's interior. Without scale numbers, names and/or units, to make clickable templates. Without scale numbers, names and/or units, to make clickable templates.

  9. Pelite - Wikipedia

    en.wikipedia.org/wiki/Pelite

    Petrogenetic grid for metapelites (click to zoom). [1] [2] Each line represents a metamorphic reaction.Metamorphic facies included are: BS = Blueschist facies, EC = Eclogite facies, PP = Prehnite-Pumpellyite facies, GS = Greenschist facies, EA = Epidote-Amphibolite facies, AM = Amphibolite facies, GRA = Granulite facies, UHT = Ultra-High Temperature facies, HAE = Hornfels-Albite-Epidote facies ...