Schist

The word schist is derived from the Greek word schķzein meaning "to split", which is a reference to the ease with which schists can be split along the plane in which the platy minerals lie. Schist is a medium-grained strongly-foliated crystalline metamorphic rock, formed by dynamic metamorphism, that can be readily split into thin flakes or slabs due to the well-developed parallelism of more than 50% of the minerals present, particularly those of lamellar or elongate prismatic habit, e.g., mica and amphiboles. Individual mineral grains are discernible by the naked eye, and this property sets it apart from slate. There are many varieties of schist and they are named for the dominant mineral comprising the rock, e.g. mica schist, green schist (green because of high chlorite content), garnet schist, actinolite schist, biotite schist etc.

Schistosity is a type of foliation, characterized by the preferred orientation of elongated or platy mineral grains (which are abundant in schistose rocks). Schistosity is a result of pressure in the crust which forces the grains to align perpendicular to the force applied. This force may be compressive (in mountain ranges) or simply caused by the weight of the overlying rocks. Metamorphic reactions between minerals upon increased burial will lead to the loss of schistosity because feldspar increases in abundance as micas become unstable. This process will lead to the formation of high-grade metamorphic rock gneiss (and gneissose fabric which can be described as a poorly developed schistosity).

The mineral assemblages and textures of the schist change with the temperature and pressure of recrystallization. With increasing metamorphism, the grain size usually increases and, depending on appropriate chemical availability, minerals such as chloritoid, garnet, staurolite, cordierite, andalusite, and kyanite crystallize as large crystals (called porphyroblasts) in a foliated micaceous matrix. Many porphyroblasts contain inclusions, indicating that they crystallized by replacement of some other mineral or rock.

schist2020(7).jpg

Biotite (dark) and muscovite (silver-grey) in a micaschist from Manhattan, New York State, USA. From James St. John.



schist2020(10).jpg

Garnet micaschist. From James St. John.



schist2020(9).jpg

Tremolite schist. Balmat, Adirondack Lowlands, New York State, USA. From James St. John.



schist2020(11).jpg

Kyanite (blue) schist. From James St. John.



schist2020(2).jpg

Graphite schist from the Urals, Russia. From Sand Atlas.



schist2020(2).jpg

Muscovite-garnet-staurolite schist that contains porphyroblasts of garnet (red, equant), kyanite (blue) and staurolite (dark, elongated). From Sand Atlas.



schist2020(4).jpg

Quartz schist with perfectly parallel cleavage surfaces. Alta, Norway. From Sand Atlas.





Bibliography



• Bucher, K., & Grapes, R. (2011). Petrogenesis of metamorphic rocks. Springer Science & Business Media.
• Fossen, H. (2016). Structural geology. Cambridge University Press.
• Howie, R. A., Zussman, J., & Deer, W. (1992). An introduction to the rock-forming minerals (p. 696). Longman.
• Passchier, Cees W., Trouw, Rudolph A. J: Microtectonics (2005).
• Philpotts, A., & Ague, J. (2009). Principles of igneous and metamorphic petrology. Cambridge University Press.
• Shelley, D. (1993). Igneous and metamorphic rocks under the microscope: classification, textures, microstructures and mineral preferred-orientations.
• Vernon, R. H. & Clarke, G. L. (2008): Principles of Metamorphic Petrology. Cambridge University Press.
• Vernon, R. H. (2018). A practical guide to rock microstructure. Cambridge university press.


Photo
micascistopiegato0097(2).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(3).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(4).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(5).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(6).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(7).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(8).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(9).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 2x (Field of view = 7mm)
micascistopiegato0097(1).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). XPL image, 2x (Field of view = 7mm)
micascisto628(22).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
micascisto628(23).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
micascisto628(24).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
micascisto628(25).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
micascisto628(26).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
micascisto628(28).jpg

Folded lepidoblastic muscovite-biotite layers and quartz layers in a mica-schist. Capo Spartivento, Calabria (Italy). PPL image, 1,25x (Field of view = 9mm)
apuane0109(14).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(16).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(17).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(18).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(19).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(20).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(21).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(22).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(23).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(24).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(25).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
apuane0109(26).jpg

lepidoblastic, crenulated muscovite layers and quartz layers in a mica-schist. Rocchetta, Apuan Alps (Italy). XPL image, 2x (Field of view = 7mm)
micascisto1162(7).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto1162(8).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto1162(9).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto1162(10).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. XPL image, 2x (Field of view = 7mm)
micascisto1162(11).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto1162(12).jpg

lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto0093(37).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto0093(38).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. XPL image, 2x (Field of view = 7mm)
micascisto0093(39).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto0093(40).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. XPL image, 2x (Field of view = 7mm)
micascisto0093(41).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. PPL image, 2x (Field of view = 7mm)
micascisto0093(42).jpg

Deformed lepidoblastic muscovite-biotite layers in a mica-schist. XPL image, 2x (Field of view = 7mm)