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Showing 1 to 5 of 5 for “"Ultrabasic rocks"”.

  1. Platinum-group elements in the ultrabasic rocks of the Braganca and Morais massifs, northern Portugal

    The ultrabasic rocks studied in this thesis are located in the Upper Allochthonous Thrust Complex nappes of the Braganca and Morais massifs, Träs-os-Montes, N. Portugal. They are relicts of residual mantle and cumulates formed at a destructive continental margin. In the Braganca massif, the …

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  2. Petrology of the Ashe Formation, Shortt's Knob area, Floyd County, Virginia

    … and studied petrographically and chemically. The rocks have been metamorphosed into the lowermost amphibolite facies and folded. The gross structure is homoclinal, generally N 80° E, >50°SE. Amphibolites (39%), chlorite schists (8%), and quartzofeldspathic schists and gneisses (53%) are the major …

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