Megacryst

Megacrystic porphyroblasts in metasomatised Quartenschiefer (metapelitic unit in the Alps)

In geology, a megacryst is a crystal or grain that is considerably larger than the encircling matrix. They are found in igneous and metamorphic rocks.[1] Megacrysts can be further classified based on the nature of their origin, either as:[2]

  • Phenocrysts, which crystallize in molten rock material (lava or magma) and are hence an earlier crystallization than the matrix in which they are embedded
  • Porphyroblasts, which develop in solid rock as the result of metamorphism or metasomatism


See also

  • Xenolith, an inclusion of one rock type in another

References

  1. ^ "Glossary of terms". Memphis Archaeological and Geological Society. 7 April 2006. Retrieved 29 December 2009.
  2. ^ Chapman, Carleton A. (2014). Phenocryst. In AccessScience. McGraw-Hill Education. https://doi.org/10.1036/1097-8542.506500

Notes

  • Significance of k-feldspar megacryst size and distribution in the tuolumne intrusive suite, California
  • v
  • t
  • e