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) |
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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: |
05 Dec 2022 14:33 |
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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