Very low-grade secondary minerals as indicators of palaeo-hydrothermal systems in the Upper Cretaceous volcanic succession of Hannah Point, Livingston Island, Antarctica-Reference-Cited by-同舟云学术

Very low-grade secondary minerals as indicators of palaeo-hydrothermal systems in the Upper Cretaceous volcanic succession of Hannah Point, Livingston Island, Antarctica

Published:2016-12 Issue: Volume:134 Page:246-256
ISSN:0169-1317
Container-title:Applied Clay Science
language:en
Short-container-title:Applied Clay Science

Author:

Bastias Joaquin^ORCID,Fuentes Francisco,Aguirre Luis,Hervé Francisco,Demant Alain,Deckart Katja,Torres Teresa

Funder

Chilean Antarctic Institute

CONICYT

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference47 articles.

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3. Very low-grade hydrothermal metamorphism of basic igneous rocks;Alt,1999

4. Estudio geomorfológico y geológico en las Islas Shetands del Sur, Antártica;Araya,1965

5. Zeolites and mafic phyllosilicates in Livingston Island, Antarctica;Bastias,2013

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