Arc and backarc geochemical signatures of the proto-Philippine Sea Plate: Insights from the petrography and geochemistry of the Samar Ophiolite volcanic section

• Published in: Journal of Asian earth sciences 2017-07, Vol.142, p.77-92
• Main Authors: Guotana, Juan Miguel R., Payot, Betchaida D., Dimalanta, Carla B., Ramos, Noelynna T., Faustino-Eslava, Decibel V., Queaño, Karlo L., Yumul, Graciano P.
• Format: Article
• Language: English
• Subjects: Backarc; Central Philippines; Mesozoic lithospheric fragments; Proto-Philippine Sea Plate; Subduction zone
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2016.07.031

•The Samar Ophiolite volcanic rocks exhibit supra-subduction zone (SSZ) signatures.•The SSZ signature is more evident in the southern ophiolites of eastern Philippines.•The Samar Ophiolite forms part of the Cretaceous proto-Philippine Sea Plate.•Fragments of the proto-Philippine Sea Plate show arc and backarc signatures. Remnants of a Cretaceous lithosphere are found at the peripheries of the West Philippine Basin. These Mesozoic fragments preserve arc affinity and include the Amami Plateau, the East Halmahera Ophiolite and the ophiolites along the eastern margin of the Philippine archipelago. The eastern margin of the Philippines is composed of Early to Late Cretaceous ophiolites and ophiolitic complexes that exhibit strong subduction imprints. The early Late Cretaceous Samar Ophiolite in the central Philippines forms part of this eastern belt. Recent surveys in southern Samar revealed the presence of peridotites, gabbros, and massive and pillowed flows of the Samar Ophiolite. Major, trace and rare earth element signatures of the volcanic rock samples indicate moderate to strong subduction-related influences and formation in an island arc setting. In contrast to other similarly-aged ophiolites along the eastern margin of the archipelago, those to the north of Samar Island exhibit weak to almost mid-oceanic ridge characteristics. These differences in the geochemical signatures of the ophiolites and ophiolitic complexes along eastern Philippines require a re-evaluation of a previous model suggesting that these ophiolites originated from a single oceanic lithosphere, possibly the proto-Philippine Sea Plate.