Zeolitización de rocas andesíticas
DOI:
https://doi.org/10.3989/egeol.89455-6501Keywords:
zeolites, hydrothermal alteration, andesitesAbstract
The study of some andesites from King George Island (South Shetland Islands, Anctartica) has pointed out the existence of a hydrothermal alteration process going rise to a zeolitic secondary minerals of low-temperature assemblages. Two paragenesis have been identified (Smectite-Bytownite-Mordenite, Smectite-Albite-Laumontite) which reflecting different conditions durign the hydrothermal alteration of these andesitic rocks
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