Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6191
Authors: Etiope, G* 
Zwahlen, C.* 
Anselmetti, F. S.* 
Kipfer, R.* 
Schubert, C. J.* 
Title: Origin and flux of a gas seep in the Northern Alps (Giswil, Switzerland)
Journal: Geofluids 
Series/Report no.: 4/ 10 (2010)
Publisher: Blackwell Publishing Ltd
Issue Date: 2010
DOI: 10.1111/j.1468-8123.2010.00302.x
Keywords: Alps
isotopes
methane
organic geochemistry
seeps
Switzerland
Subject Classification04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistry 
Abstract: Natural gas seeps in the Alpine region are poorly investigated. However, they can provide useful information regarding the hydrocarbon potential of sedimentary Alpine units and related geofluid migration, typically controlled by pressurized gas accumulations and tectonics. A gas seep located near Giswil, in the Swiss Northern Alps, was investigated, for the first time, for molecular and isotopic gas composition, methane flux to the atmosphere, and gas flux variations over time. The analyses indicated that the gas was thermogenic (CH4 > 96%; d13C1: )35.5& to )40.2&) and showed evidence of subsurface petroleum biodegradation (13C-enriched CO2, and very low C3+ concentrations). The source rock in the region is marine Type II kerogen, which is likely the same as that providing thermogenic gas in the nearby Wilen shallow well, close to Lake Sarnen. However, the lack of d13CCO2 and d13C3 data for that well prevented us from determining whether the Wilen and Giswil seeps are fed by the same reservoir and seepage system. Gas fluxes from the Giswil seep, measured using a closedchamber system, were significant and mainly from two major vents. However, a substantial gas exhalation from the soil occurs diffusely in an area of at least 115 m2, leading to a total CH4 output conservatively estimated to be at least 16 tonnes per year. Gas flux variations, monitored over a 1-month period by a special tent and flowmeter, showed not only daily meteorological oscillations, but also an intrinsic ‘pulsation’ with periods of enhanced flux that lasted 2–6 h each, occurring every few days. The pulses are likely related to episodes of gas pressure build-up and discharge along the seepage system. However, to date, no relationship to seismicity in the active Sarnen strike-slip fault system has been established.
Appears in Collections:Article published / in press

Files in This Item:
File Description SizeFormat Existing users please Login
Article.pdf1.43 MBAdobe PDF
Show full item record

WEB OF SCIENCETM
Citations 20

12
checked on Feb 10, 2021

Page view(s) 50

199
checked on Jul 17, 2024

Download(s)

30
checked on Jul 17, 2024

Google ScholarTM

Check

Altmetric