Mazurek, Martin; Waber, H.N.; Gautschi, A. (1998). Hydrocarbon gases and fluid evolution in very low-grade metamorphic terranes: A case study from the Central Swiss Alps. In: Arehart, G.B.; Hulston, J.R. (eds.) 9th Internat. Symposium on Water-Rock Interaction WRI-9 1 (pp. 417-420). New Zealand: A.A. Balkema Publisher
Full text not available from this repository.In a marl formation that was subjected to low-temperature metamorphism, free gases and groundwaters were sampled and compared with the bulk and isotopic compositions of fluid inclusions. Results indicate different sources for gas (derived thermally from kerogen) and water (which represents a mixture of connate and metamorphic water). No indications exist for later interactions of the rocks with meteoric waters.
Item Type: |
Conference or Workshop Item (Paper) |
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Division/Institute: |
08 Faculty of Science > Institute of Geological Sciences |
UniBE Contributor: |
Mazurek, Martin, Waber, Niklaus |
Subjects: |
500 Science > 550 Earth sciences & geology |
ISBN: |
90-5410-942-4 |
Publisher: |
A.A. Balkema Publisher |
Language: |
English |
Submitter: |
Niklaus Waber |
Date Deposited: |
07 Jun 2017 15:41 |
Last Modified: |
05 Dec 2022 15:06 |
Web of Science ID: |
000073721700097 |
URI: |
https://boris.unibe.ch/id/eprint/101195 |