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Saxum metamorphicum

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Gneissum, saxum metamorphicum

Saxum metamorphicum[1] vel lapis metamorphicus est lapis, qui in cortice Telluris metamorphismo producitur. Cortice mota saxa sedimentaria et saxa ignea temperatura altissima vel pressione vel aliqua solutione aquosa vel gasosa afficiuntur et mutantur.

Mica, gneissum, marmor, quartzites, schistus saxa metamorphica sunt.

Notae

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  1. ↑ Adriani Constantini Christiani Frederici van Winter Disputatio geologica inauguralis de metamorphicorum saxorum..., Lugduni Batavorum 1844, pp. 1, 46; Ioannis ab Hallwyl De saxorum et imprimis Montis Albi iugorum structura Berolini 1858, p. 14 etc.

Bibliographia

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  • Myron G. Best: Igneous and Metamorphic Petrology. W.H. Freemann & Company, Franciscopoli 1982, P. 341 sq.
  • Douglas Fettes & Jacqueline Desmons: Metamorphic Rocks: A Classification and Glossary of Terms. Cambridge University Press, Cantabrigiae 2007,
  • Wolfhard Wimmenauer: Petrographie der magmatischen und metamorphen Gesteine. Enke Verlag, Stuttgardiae 1985,

Nexus externi

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  • Atlas of Metamorphic Rocks (Anglice)


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