Stable isotope evidence for near-surface, low-temperature formation of Mg-(hydro)carbonates in highly altered Greek Mesozoic serpentinites

Andrews, Julian, Stamatakis, Michael, Mitsis, Ioannis, Donnelly, Terry, Gonzalez-Barros, M Reguerio y and Fallick, Anthony (2018) Stable isotope evidence for near-surface, low-temperature formation of Mg-(hydro)carbonates in highly altered Greek Mesozoic serpentinites. Journal of the Geological Society, 175 (2). pp. 361-375. ISSN 0016-7649

Preview

PDF (Accepted manuscript) - Accepted Version Download (3MB) | Preview

Abstract

Authigenic magnesite, hydromagnesite and huntite associated with intensely altered and serpentinized ophiolitic rocks in Attica (mainland Greece) occur predominantly as veinlets and nodules within a totally weathered former-serpentinite groundmass. Carbonate δ18O values are consistent with post-geothermal fluid temperatures between 25-70 ˚C, but mostly between 25-30 ˚C, from a dominantly meteoric-sourced groundwater, indicating near-surface, low-temperature conditions. Despite the proximity of a volcanic centre with strong CO2 flux, 75% of the carbon isotope data imply little or no incorporation of this CO2 into the authigenic Mg-(hydro)carbonates. Indeed, many δ13C values are more negative than soil-zone calcrete values, and in this setting Mg-(hydro)carbonate δ13C below -6‰ VPDB probably indicate disequilibrium effects in alkaline groundwaters. Geothermal fluids and groundwaters were mainly routed through structural conduits. Some of the low temperature hydromagnesite subsequently dehydrated to magnesite under near-surface conditions, while huntite is likely a diagenetic transformation of hydromagnesite, forming close to the volcanic centre where fluid Mg/Ca ratios were low. The isotopic signatures are distinct from previously published Balkan-East Mediterranean magnesite data arrays but are consistent with many other ultramafic-associated magnesium carbonates worldwide; their association with likely fluid compositions provide important context for Mg-(hydro)carbonate formation as geothermal conditions cool to near surface temperatures.

Item Type:	Article
Faculty \ School:	Faculty of Science > School of Environmental Sciences
UEA Research Groups:	Faculty of Science > Research Groups > Geosciences
Depositing User:	Pure Connector
Date Deposited:	15 Nov 2017 06:06
Last Modified:	15 May 2025 00:01
URI:	https://ueaeprints.uea.ac.uk/id/eprint/65449
DOI:	10.1144/jgs2017-083

Downloads

Actions (login required)

View Item