Abstract
THE presence of dissolved water can significantly change the sequence in which different minerals crystallize from a silicate magma1–3. This will alter the compositional path followed by residual liquids (the liquid line of descent'), and modify the types and compositions of crystals that accumulate at the site of cooling. The sharp decrease in the solubility of water in silicate melts with decreasing pressure makes direct measurements of pre-eruptive concentrations in magmas difficult because much of the dissolved water boils off before eruption. Here we report experimental results on the crystallization of basalts that contain substantial dissolved water (up to 6 wt%), and show how the results can be used to infer the amount of dissolved H2O involved in the petrogenesis of lavas that preserve a record of their liquid lines of descent, or the accumulated minerals left behind after solidification. The presence of abundant magmatic water is a signature of subduction-zone volcanism4, and can be used to associate a suite of magmas or igneous cumulates with a convergent-margin, back-arc or interarc tectonic setting.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Holloway, J. R. & Burnham, C. W. J. Petrology 13, 1–29 (1972).
Kushiro, I. Am. J. Sci. 267A, 269–294 (1969).
Nicholls, I. A. & Ringwood A. E. J. Geol. 81, 285–300 (1973).
White, D. & Waring G. A. Prof. Paper No. 440K, 1–29 (US Geol. Survey, Washington DC, 1963).
Perfit, M. R., Gust, D. A., Bence, A. E., Arculus, R. J. & Taylor, S. R. Chem. Geol. 30, 227–256 (1980).
Melson, W. G., Thompson, G. & van Andel, Tj. H. J. geophys. Res. 73, 5925–5941 (1968).
Elthon, D., Casey, J. F. & Komor, S. J. geophys. Res. 87, 8717–8734 (1982).
Gust, D. A. & Perfit, M. R. Contr. Miner. Petrol. 97, 7–18 (1987).
Gaetani, G. A., Grove, T. L. & Bryan, W. B. Proc. ODP Sci. Res. (in the press).
Walker, D., Shibata, T. & DeLong, S. E. Contr. Miner. Petrol. 70, 111–125 (1979).
Grove, T. L., Gerlach, D. C. & Sando, T. W. Contr. Miner. Petrol. 80, 160–182 (1982).
Grove, T. L., Kinzler, R. J. & Bryan, W. B. Mantle Flow and Melt Generation at Mid-Ocean Ridges 281–310 (Am. geophys. Un., Washington DC, 1993).
Bender, J. F., Hodges, F. N. & Bence, A. E. Earth planet. Sci. Lett. 41, 277–302 (1978).
Green, D. H., Hibberson, W. O. & Jaques, A. L. The Earth: It's Origin, Structure, and Evolution 265–299 (Academic, London, 1979).
Yoder, H. S. Carnegie Inst. Washington Yb. 64, 82–89 (1965).
Sisson, T. W. & Grove, T. L. Contr. Miner. Petrol. 113, 143–166, 167–184 (1993).
Barsdell, M. J. Petrology 29, 927–964 (1988).
Barsdell, M. & Berry, R. F. J. Petrology 31, 747–777 (1990).
Foden, J. D. J. Petrology 24, 98–130 (1983).
Eggins, S. M. Contr. Miner. Petrol. 114, 79–100 (1993).
Thirwall, M. F. & Graham, A. M. J. geol. Soc. Lond. 141, 427–445 (1984).
Marsh, B. D. J. Geol. 84, 27–45 (1976).
Marsh, B. D. Andesites 99–114 (Wiley, New York, 1982).
Kay, S. M. & Kay, R. W. Contr. Miner. Petrol. 90, 276–290 (1985).
Brophy, J. G. Contr. Miner. Petrol. 93, 368–380 (1986).
Myers, J. D., Marsh, B. D. & Sinha, A. K. Contr. Miner. Petrol. 94, 1–11 (1986).
Nye, C. J. & Reid, M. R. J. geophys. Res. 91, 10271–10287 (1986).
Debari, S., Kay, S. M. & Kay, R. W. J. Geol. 95, 329–341 (1987).
Bartels, K. S., Kinzler, R. J. & Grove, T. L. Contr. Miner. Petrol. 108, 253–270 (1991).
Grove, T. L., Kinzler, R. J. & Bryan, W. B. Proc. ODP Sci. Res. 106/109, 9–17 (1990).
Conrad, W. K. & Kay, R. W. J. Petrology 25, 88–125 (1984).
Wilshire, H. G. et al. Prof. Paper No. 1443, 111 (US Geol. Survey, Reston, Virginia, 1988).
Wilkinson, J. F. G. Contr. Miner. Petrol. 58, 181–201 (1976).
Komor, S. C., Elthon, D. & Casey, J. F. J. geophys. Res. 90, 7705–7736 (1985).
Pallister, J. S. & Hopson, C. A. J. geophys. Res. 86, 2593–2644 (1981).
Ernewein, M., Pflumio, C. Whitechurch, H. Tectonophysics 151, 247–274 (1988).
Irvine, T. N. Geol. Soc. Am. Memoir No. 138, 240 (Geol. Soc. Am., Boulder, 1974).
Snoke, A. W., Quick, J. E. & Bowman, H. R. J. Petrology 22, 501–552 (1981).
Sivell, W. & Rankin, P. N. Z J. Geol. Geophys. 26, 239–257 (1983).
Elthon, D. Nature 354, 140–143 (1991).
Tormey, D. R., Grove, T. L. & Bryan, W. B. Contr. Miner. Petrol. 96, 121–139 (1987).
Kinzler, R. J. & Grove, T. L. J. Geophys. Res. 97, 6885–6906 (1992).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Gaetani, G., Grove, T. & Bryan, W. The influence of water on the petrogenesis of subductionrelated igneous rocks. Nature 365, 332–334 (1993). https://doi.org/10.1038/365332a0
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/365332a0
This article is cited by
-
Textural and compositional zoning in plagioclase phenocrysts: implications for magma chamber processes in the Emeishan large Igneous Province, SW China
Acta Geochimica (2023)
-
Petrogenetic insights from relict augites in Neoarchean Kotima basalt of Dongargarh Supergroup, Bastar Craton, Central India
Journal of Earth System Science (2022)
-
Petrogenesis of Neoarchean Mangikhuta Volcanic Complex, Dongargarh Supergroup, Central India: Insights from Relict Clinopyroxene Chemistry
Journal of the Geological Society of India (2020)
-
Early Cretaceous bimodal volcanic rocks in the Yinshan belt, North China Craton: age, petrogenesis, and geological significance
International Journal of Earth Sciences (2020)
-
The contrasting geochemical message from the New Caledonia gabbronorites: insights on depletion and contamination processes of the sub-arc mantle in a nascent arc setting
Contributions to Mineralogy and Petrology (2018)
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.