Titlebook: Ophiolite Genesis and Evolution of the Oceanic Lithosphere; Proceedings of the O Tj. Peters,A. Nicolas,R. G. Coleman Conference proceedings

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https://doi.org/10.1007/978-94-011-3358-6Coast; Ocean; dike; fault; igneous rock; marine; obduction; subduction; tectonics

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978-94-010-5484-3Ministry of Petroleum and Minerals, Sultanate of Oman 1991

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Ophiolite Genesis and Evolution of the Oceanic Lithosphere978-94-011-3358-6Series ISSN 0924-1957

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Introductionphiolites has provided a wealth of insight into lithospheric processes and has proved to be an indispensible prerequisite to interpreting geophysical and other investigations of the crust underlying recent oceans. The Oman Ophiolite offers the most complete and structurally undisturbed sections of t

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Platinum-Group Elements and Gold in Ophiolitic Complexes: Distribution and Fractionation from Mantlep Elements (PGE) are nearly unfractionated in the less depleted mantle rocks (lherzolites). Residual dunites are clearly empoverished in Pt, Pd, and Au which were collected by silicate melts during partial melting. The chromite grains of the podiform chromitites, which crystallized early in magmatic

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Chromite-Rich and Chromite-Poor Ophiolites: The Oman Casectonically rotated to become parallel to the peridotite foliation. This occurred soon after their formation within the transition zone below the ridge of origin. Subconcordant and discordant pods are also present. The latter have preserved delicate magmatic structures showing that they have only bee

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