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

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

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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.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences
08 Faculty of Science > Institute of Geological Sciences > Rock-Water Interaction

UniBE Contributor:

Waber, Niklaus

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

1878-5220

Publisher:

Elsevier

Language:

English

Submitter:

Niklaus Waber

Date Deposited:

18 Aug 2014 09:13

Last Modified:

30 Jan 2017 16:22

Publisher DOI:

10.1016/j.proeps.2013.03.126

Uncontrolled Keywords:

natural tracers, solute transport, chlorine isotopes, porewater

BORIS DOI:

10.7892/boris.49898

URI:

https://boris.unibe.ch/id/eprint/49898

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