Assessing Initial Conditions for Chloride Transport Across Low- permeability Argillaceous Rocks, Wellenberg, Switzerland


Autoria(s): Waber, Niklaus; Hobbs, M.Y.; Frape, S.K.
Data(s)

2013

Resumo

Information about fluid evolution and solute transport in a low-permeability metamorphic rock sequence has been obtained by comparing chloride concentrations and chlorine isotope ratios of pore water, groundwater, and fluid inclusions. The similarity of d37Cl values in fluid inclusions and groundwater suggests a closed-system evolution during the metamorphic overprint, and signatures established at this time appear to form the initial conditions for chloride transport after exhumation of the rock sequence.

Formato

application/pdf

Identificador

http://boris.unibe.ch/49898/1/Waber_Hobbs.pdf

Waber, Niklaus; Hobbs, M.Y.; Frape, S.K. (2013). Assessing Initial Conditions for Chloride Transport Across Low- permeability Argillaceous Rocks, Wellenberg, Switzerland. Procedia Earth and Planetary Science, 7, pp. 875-879. Elsevier 10.1016/j.proeps.2013.03.126 <http://dx.doi.org/10.1016/j.proeps.2013.03.126>

doi:10.7892/boris.49898

info:doi:10.1016/j.proeps.2013.03.126

urn:issn:1878-5220

Idioma(s)

eng

Publicador

Elsevier

Relação

http://boris.unibe.ch/49898/

Direitos

info:eu-repo/semantics/openAccess

Fonte

Waber, Niklaus; Hobbs, M.Y.; Frape, S.K. (2013). Assessing Initial Conditions for Chloride Transport Across Low- permeability Argillaceous Rocks, Wellenberg, Switzerland. Procedia Earth and Planetary Science, 7, pp. 875-879. Elsevier 10.1016/j.proeps.2013.03.126 <http://dx.doi.org/10.1016/j.proeps.2013.03.126>

Palavras-Chave #550 Earth sciences & geology
Tipo

info:eu-repo/semantics/article

info:eu-repo/semantics/publishedVersion

PeerReviewed