Petrochemical Investigation of the Antique Ophiolite (Philippines): Implications on Volcanogenic Massive Sulfide and Podiform Chromitite Deposits
Identifieur interne : 003671 ( Main/Exploration ); précédent : 003670; suivant : 003672Petrochemical 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 :
- Resource Geology [ 1344-1698 ] ; 2001-06.
Descripteurs français
- Wicri :
- geographic : Philippines.
English descriptors
- KwdEn :
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:
- Colombie, France
- Midi-Pyrénées, Occitanie (région administrative), Région Bretagne
- Brest, Toulouse
- Université Toulouse III - Paul Sabatier, Université de Bretagne Occidentale
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 001225
- to stream Istex, to step Curation: 001223
- to stream Istex, to step Checkpoint: 000E82
- to stream Main, to step Merge: 003C49
- to stream Main, to step Curation: 003671
Le document en format XML
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<front><div type="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.</div>
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