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• W2045592502 abstract "Masirah Island is almost entirely composed of a highly faulted and unmetamorphosed folded ophiolite complex which is unconformably overlain by unfolded Eocene limestone and is correlated with the Upper Cretaceous Semail Complex of the Oman Mainland. The ophiolites include serpentine, basalt, pyroclastics and some radiolarite, and intrusive complexes largely composed of serpentine, peridotite, picrite, anorthosite, gabbro and granite, with transitional varieties. Emplacement structures within the intrusions are extremely complicated, with the gabbros full of blocks mostly of serpentine up to 1 km or more in diameter. There are also late stage veins, lenses and irregular bodies of granite. Ophiolites, probably derived from the mantle, are ultrabasic differentiates with soda metasomatism. Tectonic structures are largely pre-Eocene. They include fractures, some of which are parallel to the late Tertiary submarine Masirah fault which is related to continental drift. L'ǐle de Masirah se compose entièrement d'un complexe ophiolite plissé, démétamorphosé et à failles multiples, qui est recouvert en discordance de calcaire Eocène sans plissement et qui est corrélatif au complexe Semail Crétacé supérieur de la contrée d'Oman. Les ophiolites comprennent serpentine, basalte, pyroclastiques et de quelques radiolarites et des complexes intercalés largement composés de serpentine, periodotite, picrite, anorthosite, gabbro et granite et des variétés de transition. Les structures d'emplacement à l'intérieur des intrusions sont extrěmement compliquées dont les gabbros sont pleins de blocs qui sont principalement de serpentine qui ont jusqu' à 1 km ou plus de diamètre. Il y a aussi des veines et des corps de granite de formation plus récente. Ophiolìtes probablement dérivés du manteau sont fractions ultrabasiques avec métasomatisme de soudure. Les structures tectoniques sont en grande partie pré-Eocène. Elles comprennent des fractures dont quelques - unes sont parallèles à la faille sous - marine de Masirah du Tertiaire supérieur, qui est rattachée à la Dérive des Continents." @default.
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• W2045592502 date "2007-04-30" @default.
• W2045592502 modified "2023-09-24" @default.
• W2045592502 title "The upper cretaceous ophiolite complex of Masirah Island, Oman" @default.
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• W2045592502 doi "https://doi.org/10.1002/gj.3350060211" @default.
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