Geochemistry of H- and CH-enriched hydrothermal fluids of Socorro Island, Revillagigedo Archipelago, Mexico. Evidence for serpentinization and abiogenic methane Y. A. TARAN et al. Socorro hydrocarbons.

Taran, Y. A.; Varley, N. R.; Inguaggiato, S.; Cienfuegos, E.

Socorro Island is the exposed part of an approx. 4000-m-high volcanic edifice rising from the oceanic floor to approx. 1000 m asl at the northern part of the Mathematician Ridge, Eastern Pacific. The volcano is active, with the most recent basaltic eruption in 1993. Moderate fumarolic activity and diffuse degassing with a total CO flux of approx. 20 total day are concentrated in the summit region of the volcano composed of a group of rhyolite domes. Low-temperature, boiling point, fumaroles discharge gas with high H (up to 20 mol% in dry gas) and CH (up to 4 mol%). Both carbon and He isotopic ratios and abundances correspond to those in MORB fluids (δ≈−5‰; He/He = 7.6 R, CO/He = (2-3) × 10, where R is the atmospheric ratio He/He of 1.4 × 10). Light hydrocarbons (CH, CH, CH, and CH) are characterized by a high C/C ratio of approx. 1000. Methane is enriched in C (δ from −15 to −20‰) and H (δH from −80 to −120‰), and hydrocarbons show an inverse isotopic trend in both δC and δH (ethane is isotopically lighter than methane). These isotopic and concentration features of light hydrocarbons are similar to those recently discovered in fluids from ultramafic-hosted spreading ridge vents and may be related to the serpentinization processes: H generation and reduction of CO to CH within high-temperature zone of volcano-seawater hydrothermal system hosted in basaltic and ultramafic rocks beneath a volcano edifice. The thermodynamic analysis of this unusual composition of the Socorro fluids and the assessment of endmember compositions are complicated by the near-surface cooling, condensation and mixing with meteoric water.

SOCORRO Island (Mexico); MEXICO; GEOCHEMISTRY; VOLCANIC eruptions -- Environmental aspects; METHANE; HYDROCARBONS

Geofluids, 2010, Vol 10, Issue 4, p542

1468-8115

Academic Journal

10.1111/j.1468-8123.2010.00314.x