Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia

M. A. Lanphere; R. G. Coleman; S. Karamata; J. Pamic

doi:10.1016/0012-821x(75)90001-1

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Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia

M. A. Lanphere·R. G. Coleman·S. Karamata·J. Pamic

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Abstract

Amphibolites associated with alpine peridotites in the Central Ophiolite zone in Yugoslavia have K-Ar ages of 160–170 m.y. These amphibolites and associated peridotites underwent deep-seated metamorphism prior to tectonic emplacement into the sedimentary-volcanic assemblage of the Dinarides. The alpine peridotites and associated local rocks of the ophiolite suite are interpreted as Jurassic oceanic crust and upper mantle.

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Earth and Planetary Science Letters Article

Source-reported bounding extent: 40.64730356252251° to 46.49839225859763° latitude; 17.7978515625° to 26.71875° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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M. A. Lanphere, R. G. Coleman, S. Karamata, J. Pamic. 1975. Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia. https://doi.org/10.1016/0012-821x(75)90001-1

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