Insights into mantle-type volatiles contribution from dissolved gases in artesian waters of the Great Artesian Basin, Australia

Italiano F., Yuce G., Uysal I. T., Gasparon M., Morelli G.

CHEMICAL GEOLOGY, vol.378, pp.75-88, 2014 (SCI-Expanded) identifier identifier

  • Publication Type: Article / Article
  • Volume: 378
  • Publication Date: 2014
  • Doi Number: 10.1016/j.chemgeo.2014.04.013
  • Journal Name: CHEMICAL GEOLOGY
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Page Numbers: pp.75-88
  • Hacettepe University Affiliated: Yes


The geochemical features of the volatiles dissolved in artesian thermal waters discharged over three basins (Millungera, Galilee and Cooper basin) of the Australian Great Artesian Basin (GAB) consistently indicate the presence of fluids from multiple gas sources located in the crust (e.g. sediments, oil reservoirs, granites) as well as minor but detectable contributions of mantle/magma-derived fluids. The gases extracted from 19 water samples and analyzed for their chemical and isotopic composition exhibit amounts of CO2 up to about 340 mlSTP/L-H2O marked by a delta C-13(TDc) (Total Dissolved Carbon) ranging from - 16.9 to + 0.18 parts per thousand vs PDB, while CH4 concentrations vary from 4.4 x 10(-5) to 4.9 mlSTP/L-H2O. Helium contents were between 9 and >2800 times higher than equilibrium with Air Saturated Water (ASW), with a maximum value of 0.12 mlSTP/L-H2O. Helium isotopic composition was in the 0.02-0.21 Ra range (Ra = air-normalized He-3/He-4 ratio). The three investigated basins differ from each other in terms of both chemical composition and isotopic signatures of the dissolved gases whose origin is attributed to both mantle and crustal volatiles. Mantle He is present in the west-central and hottest part of the GAB despite no evidence of recent volcanism. We found that the partial pressure of helium, significantly higher in crustal fluids than in mantle-type volatiles, enhances the crustal He signature in the dissolved gases, thus masking the original mantle contribution. Neotectonic activity involving deep lithospheric structures and magma intrusions, highlighted by recent geophysical investigations, is considered to be the drivers of mantle/magmatic volatiles towards the surface. The results, although pertaining to artesian waters from a vast area of >542,000 km(2), provide new constraints on volatile injection, and show that fluids' geochemistry can provide additional and independent information on the geo-tectonic settings of the Great Artesian Basin and its geothermal potential. (C) 2014 Elsevier B.V. All rights reserved.