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migmatite
EntityQ744630· pop 37· linked from 379 articles

thumb|Ptygmatic folding in migmatite on Naissaar Island, Estonia thumb|Migmatite on the coast of Saaremaa, Estonia thumb|Intricately-folded migmatite from near Geirangerfjord, Norway

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Migmatite
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~16 min read

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12 sections
Contents
  • The diagenesis - metamorphism sequence
  • Partial melting, anatexis and the role of water
  • Color-banded migmatites
  • Migmatite textures
  • Early history of migmatite investigations
  • Agmatite
  • Migmatite melts provide buoyancy for sedimentary isostasy
  • Other migmatite hypotheses
  • Etymology
  • See also
  • References
  • External links

thumb|Ptygmatic folding in migmatite on Naissaar Island, Estonia thumb|Migmatite on the coast of Saaremaa, Estonia thumb|Intricately-folded migmatite from near Geirangerfjord, Norway

Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian cratonic blocks. It consists of two or more constituents often layered repetitively: one layer is an older metamorphic rock that was reconstituted subsequently by partial melting ("paleosome"), while the alternate layer has a pegmatitic, aplitic, granitic or generally plutonic appearance ("neosome"). Commonly, migmatites occur below deformed metamorphic rocks that represent the base of eroded mountain chains.

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