Articles | Volume 11, issue 20
Research article
16 Oct 2014
Research article |  | 16 Oct 2014

Fluid chemistry of the low temperature hyperalkaline hydrothermal system of Prony Bay (New Caledonia)

C. Monnin, V. Chavagnac, C. Boulart, B. Ménez, M. Gérard, E. Gérard, C. Pisapia, M. Quéméneur, G. Erauso, A. Postec, L. Guentas-Dombrowski, C. Payri, and B. Pelletier

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Cited articles

Arcilla, C. A., Pascua, C. S., and Alexander, W. R.: Hyperalkaline groundwaters and tectonism in the Philippines: significance to natural Carbon Capture and Sequestration, in: 10th International Conference on Greenhouse Gas Control Technologies, Energy Procedia, edited by: Gale, J., Hendriks, C. and Turkenberg, W., 5093–5101, 2011.
Avias, J.: Overthrust structure of the main ultrabasic new caledonian massives, Tectonophysics, 4, 531–541, 1967.
Barnes, I. and O'Neil, J.: The relationship between fluids in some fresh alpine-type ultramafics and possible modern serpentinization, Western United States, Geol. Soc. Am. Bull., 80, 1947–1960, 1969.
Barnes, I., O'Neil, J. R., and Trescases, J. J.: Present day serpentinization in New Caledonia, Oman and Yugoslavia, Geochim. Cosmochim. Ac., 42, 144–145, 1978.
Bénézeth, P., Saldi, G. D., Dandurand, J.-L., and Schott, J.: Experimental determination of the solubility product of magnesite at 50 to 200 °C, Chem. Geol., 286, 21–31, 2011.
Final-revised paper