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On the genesis of aluminum-rich speleothems in a granite cave of NW Spain

Granite massifs often contain caves, with dimensions ranging from a few meters up to 1,000 m, also referred to as pseudokarst. The speleothems in such caves are mostly composed of either Si-rich (commonly opal-A) or Al-rich authigenic mineraloids. Whereas the formation and geochemical composition of...

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Detalhes bibliográficos
Principais autores: Jorge Sanjurjo-Sanchez, Carlos Arce Chamorro, Juan Ramón Vidal Romaní, Marcos Vaqueiro-Rodríguez, Victor Barrientos, Joeri Kaal
Formato: Artigo
Idioma:Inglês
Publicado em: University of South Florida Libraries 2021-01-01
coleção:International Journal of Speleology
Assuntos:
Acesso em linha:https://scholarcommons.usf.edu/ijs/vol50/iss1/3/
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