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Science 9 September 1994: Vol. 265. no. 5178, pp. 1563 - 1565 DOI: 10.1126/science.265.5178.1563
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Articles
Rapid Emplacement of Young Oceanic Lithosphere: Argon Geochronology of the Oman Ophiolite
Bradley R. Hacker 1
1 Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA.
40Ar/39Ar dates of emplacement-related metamorphic rocks beneath the Samail ophiolite in Oman show that cooling to <525°C occurred within 1 million years of igneous crystallization of the ophiolite. This unexpectedly short time span and rapid cooling means that old, cold continental or oceanic lithosphere must have been adjacent to the ophiolite during spreading and then been thrust beneath the ophiolite almost immediately afterward.
Submitted on April 22, 1994
Accepted on July 21, 1994
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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- Ophiolite obduction and the Samail Ophiolite: the behaviour of the underlying margin.
- D. R. Gray and R. T. Gregory (2003)
Geological Society, London, Special Publications
218, 449-465
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- Subduction zone polarity in the Oman Mountains: implications for ophiolite emplacement.
- M. P. Searle, C. J. Warren, D. J. Waters, and R. R. Parrish (2003)
Geological Society, London, Special Publications
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- Subduction zone metamorphism during formation and emplacement of the Semail ophiolite in the Oman Mountains.
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- R. B. Pedersen, R. B. PEDERSEN, M. P. SEARLE, and R. I. CORFIELD (2001)
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