EGU24-12897, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-12897
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

First indications on CH4 origin in the CO2-dominated gas discharges of the western Eger Rift (Czech Republic)

Walter D'Alessandro1, Kyriaki Daskalopoulou2,3, Fausto Grassa1, Andrea Vieth-Hillebrand3, Martin Zimmer3, Samuel Niedermann3, and Heiko Woith3
Walter D'Alessandro et al.
  • 1Istituto Nazionale di Geofisica e Vulcanologia, sezione di Palermo, Palermo, Italy (w.dalessandro@pa.ingv.it)
  • 2Institute of Geosciences, University of Potsdam, Potsdam, Germany
  • 3Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, Potsdam, Germany

Tectonic structures such as faults and fractures act as preferential pathways for gas ascent and their consequent release into the atmosphere. Magma-derived gases are widespread throughout the western Eger Rift (Czech Republic), an intraplate region without active volcanism but with the occurrence of mid-crustal earthquake swarms. Geogenic COdischarges from the Počatky–Plesná fault zone (PPZ), Mariánské Lázně Fault (MLF), Bad Brambach (BB), and a deep local fault (DLF) have been sampled since 2021. Gases were analysed for their chemical (CO2, N2, O2, Ar, He, CH4, and H2) and isotopic contents (noble gases, CO2, and CH4). Results showed that CO2 is the dominant gas species (concentrations > 99.4%), with the remaining gases being present in minor amounts. The He isotopic composition for gas samples from the PPZ and MLF is typical for the subcontinental lithospheric mantle (SCLM - with 3He/4He ratios between 5 and 6 RA), while gases from BB and the DLF show a lower mantle input (3He/4He is 3.2 and 2.4 RA, respectively). δ13CCO2 data reflect a SCLM CO2 signature (-4 to -1 ‰ vs. V-PDB). First CH4 isotopic data present values between -52.0 and -47.1 ‰ vs. V-PDB for δ13CCH4 and between -307 and -284 ‰ vs. V-SMOW for δ2HCH4. With the exception of samples collected from the MLF that show a clear thermogenic CH4 origin, all the other samples present isotopic values and CH4/(C2H6+C3H8) ratios that suggest a likely biogenic origin, with secondary processes playing a crucial role on the gases’ isotopic signature. It should be noted that low CH4concentrations (<100 μmol/mol) correspond to low CH4/3He ratios (around 104) in CO2-rich magmatic gases, suggesting a possible common origin for these gases. Therefore, multiple origins of CH4 (biogenic and volcanic-geothermal) cannot be excluded.

This research is a part of the MoCa - “Monitoring Carbon” project and this work was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – 461419881.

How to cite: D'Alessandro, W., Daskalopoulou, K., Grassa, F., Vieth-Hillebrand, A., Zimmer, M., Niedermann, S., and Woith, H.: First indications on CH4 origin in the CO2-dominated gas discharges of the western Eger Rift (Czech Republic), EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12897, https://doi.org/10.5194/egusphere-egu24-12897, 2024.