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Pertita

De Wikipedia, la enciclopedia libre

Crecimiento antipertítico de vetas de feldespato potásico intercaladas con vetas de feldespato sódico.

Las pertitas se originan como producto de una mezcla de feldespato potásico y plagioclasa (albita).[1]​[2]​

Durante el proceso, las pertitas se ubican de forma paralela en bandas más o menos sinuosas. Cuando ocurre en un feldespato potásico, el intercrecimiento de plagioclasa se denomina pertita. Cuando ocurre en una plagioclasa un intercrecimiento de feldespato potásico, se denomina antipertita.[1]​

Referencias

  1. ↑ a b College of Science and Technology. Central Michigan University. «Perthite» (en inglés). Archivado desde el original el 8 de junio de 2007. Consultado el 13 de julio de 2009. 
  2. ↑ Mindat.org. «Perthite» (en inglés). Consultado el 13 de julio de 2009. 
Esta página se editó por última vez el 14 abr 2022 a las 18:51.
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