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• W2735595537 endingPage "417" @default.
• W2735595537 startingPage "401" @default.
• W2735595537 abstract "Cretaceous ophiolites and ophiolitic fragments occur in the Samar and Leyte islands in eastern central Philippines. The Samar Ophiolite is a complete crust–mantle sequence exposed in southern Samar, whereas the Tacloban and Malitbog ophiolite complexes are, respectively, located in the northeastern and southwestern portions of the nearby Leyte island. Despite the close proximity of these islands, the genetic relationship of these ophiolites and ophiolitic complexes, if any, remains to be elucidated. We present here new petrographic and geochemical data on the harzburgites and dunites of the ultramafic section of the Samar Ophiolite. These mantle peridotites are highly depleted residues which have low modal pyroxene content, high spinel Cr# (=0.62–0.79), and slightly enriched light rare earth element abundance with depletion in Zr and Ti. Such characteristics are typical of supra-subduction zone peridotites and strongly contrast with the abyssal signatures of the Tacloban and Malitbog ophiolite complexes. The absence of a structure between these adjacent ophiolite fragments initially hints that they form a single oceanic crust. However, with our new results, we suggest other possible mechanisms that could explain the relationship of these ophiolites." @default.
• W2735595537 created "2017-07-21" @default.
• W2735595537 creator A5010604149 @default.
• W2735595537 creator A5021945756 @default.
• W2735595537 creator A5022741502 @default.
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• W2735595537 creator A5054411752 @default.
• W2735595537 creator A5062249426 @default.
• W2735595537 creator A5069438045 @default.
• W2735595537 date "2017-07-12" @default.
• W2735595537 modified "2023-10-18" @default.
• W2735595537 title "Petrological and geochemical characteristics of the Samar Ophiolite ultramafic section: implications on the origins of the ophiolites in Samar and Leyte islands, Philippines" @default.
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