The role of gypsum and/or dolomite dissolution in tufa precipitation: lessons from the hydrochemistry of a carbonate–sulphate karst system

This research was carried out while DDV was granted with a Juan de la Cierva fellowship from the Spanish Government.

Detalhes bibliográficos
Autores: Domínguez Villar, David, Vázquez-Navarro, Juan A., Krklec, Kristina
Formato: artículo
Estado:Versión borrador
Fecha de publicación:2016
País:España
Recursos:Universidad de Salamanca (USAL)
Repositorio:GREDOS. Repositorio Institucional de la Universidad de Salamanca
OAI Identifier:oai:dnet:gredos______::106ce0d62ea1b9fc2e1a6edc3044d2b9
Acesso em linha:http://hdl.handle.net/10366/170929
Access Level:acceso abierto
Palavra-chave:Hydrochemistry
Tufa
Calcite
Gypsum
Incongruent dissolution of dolomite
2506 Geología
Descrição
Resumo:This research was carried out while DDV was granted with a Juan de la Cierva fellowship from the Spanish Government.