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Petrochemical Investigation of the Antique Ophiolite (Philippines): Implications on Volcanogenic Massive Sulfide and Podiform Chromitite Deposits

Identifieur interne : 003671 ( Main/Exploration ); précédent : 003670; suivant : 003672

Petrochemical Investigation of the Antique Ophiolite (Philippines): Implications on Volcanogenic Massive Sulfide and Podiform Chromitite Deposits

Auteurs : Rodolfo A. Tamayo Jr ; Graciano P. Yumul Jr [Colombie] ; René C. Maury [France] ; Mireille Polvé [France] ; Joseph Cotten [France] ; Marcel Bohn [France]

Source :

RBID : ISTEX:48D042E0DF66138BD7A499D0DA64BD233AEF2027

Descripteurs français

English descriptors

Abstract

Abstract: The Antique ophiolite, located in Panay island (west‐central Philippines), corresponds to several tectonic slices within the suture zone between the Philippine Mobile Belt (PMB) and the North Palawan Block (NPB). It includes dismembered fragments of a basaltic sequence, dominantly pillow‐lavas with minor sheet flows, rare exposures of sheeted dikes, isotropic gabbros, subordinate layered mafic and ultramafic rock sequences and serpentinites. Most of the ophiolite units commonly occur as clasts and blocks within the serpentinites, which intrude the whole ophiolitic body, as well as, the basal conglomerate of the overlying Middle Miocene sedimentary formation.

Url:
DOI: 10.1111/j.1751-3928.2001.tb00088.x


Affiliations:


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