Item talk:Q161351

Geoscience Ontology Description

Rock in which calcium-bearing plagioclase feldspar is altered to an assemblage of minerals called saussurite, typically including zoisite, chlorite, amphibole, and carbonate minerals. Residual fluids present during the late stages of magmatic crystallization can react with previously formed plagioclase feldspar to form saussurite; the saussurite will be spread through the plagioclase or located near its outer margin. The plagioclase may be reconstituted into a more sodium-rich variety (albite), although the original form of the crystal is retained. Later hydrothermal alteration can produce the same result. Mafic rocks are especially susceptible to saussuritization owing to their high calcium content; the more calcium-rich portions of plagioclase in acidic rocks also are often saussuritized.