Slab rollback and microcontinent subduction in the evolution of the Zambales Ophiolite Complex (Philippines)

A review

Graciano P. Yumul, Carla B. Dimalanta, Ricky C. Salapare, Karlo L. Queaño, Decibel V. Faustino-Eslava, Edanjarlo J. Marquez, Noelynna T. Ramos, Betchaida D. Payot, Juan Miguel R. Guotana, Jillian Aira S. Gabo-Ratio, Leo T. Armada, Jenielyn T. Padrones, Keisuke Ishida, Shigeyuki Suzuki

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

New radiolarian ages show that the island arc-related Acoje block of the Zambales Ophiolite Complex is possibly of Late Jurassic to Early Cretaceous age. Radiometric dating of its plutonic and volcanic-hypabyssal rocks yielded middle Eocene ages. On the other hand, the paleontological dating of the sedimentary carapace of the transitional mid-ocean ridge – island arc affiliated Coto block of the ophiolite complex, together with isotopic age datings of its dikes and mafic cumulate rocks, also yielded Eocene ages. This offers the possibility that the Zambales Ophiolite Complex could have: (1) evolved from a Mesozoic arc (Acoje block) that split to form a Cenozoic back-arc basin (Coto block), (2) through faulting, structurally juxtaposed a Mesozoic oceanic crust with a younger Cenozoic lithospheric fragment or (3) through the interplay of slab rollback, slab break-off and, at a later time, collision with a microcontinent fragment, caused the formation of an island arc-related ophiolite block (Acoje) that migrated trench-ward resulting into the generation of a back-arc basin (Coto block) with a limited subduction signature. This Meso-Cenozoic ophiolite complex is compared with the other oceanic lithosphere fragments along the western seaboard of the Philippines in the context of their evolution in terms of their recognized environments of generation.

Original languageEnglish
JournalGeoscience Frontiers
DOIs
Publication statusPublished - Jan 1 2019

Fingerprint

ophiolite
slab
subduction
island arc
Eocene
hypabyssal rock
mid-ocean ridge
oceanic lithosphere
cumulate
basin
oceanic crust
trench
dike
volcanic rock
faulting
collision
Jurassic
Cretaceous
rock
dating

Keywords

  • Ophiolite
  • Philippines
  • Radiolarians
  • Slab rollback
  • Subduction
  • Zambales

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)

Cite this

Slab rollback and microcontinent subduction in the evolution of the Zambales Ophiolite Complex (Philippines) : A review. / Yumul, Graciano P.; Dimalanta, Carla B.; Salapare, Ricky C.; Queaño, Karlo L.; Faustino-Eslava, Decibel V.; Marquez, Edanjarlo J.; Ramos, Noelynna T.; Payot, Betchaida D.; Guotana, Juan Miguel R.; Gabo-Ratio, Jillian Aira S.; Armada, Leo T.; Padrones, Jenielyn T.; Ishida, Keisuke; Suzuki, Shigeyuki.

In: Geoscience Frontiers, 01.01.2019.

Research output: Contribution to journalArticle

Yumul, GP, Dimalanta, CB, Salapare, RC, Queaño, KL, Faustino-Eslava, DV, Marquez, EJ, Ramos, NT, Payot, BD, Guotana, JMR, Gabo-Ratio, JAS, Armada, LT, Padrones, JT, Ishida, K & Suzuki, S 2019, 'Slab rollback and microcontinent subduction in the evolution of the Zambales Ophiolite Complex (Philippines): A review', Geoscience Frontiers. https://doi.org/10.1016/j.gsf.2018.12.008
Yumul, Graciano P. ; Dimalanta, Carla B. ; Salapare, Ricky C. ; Queaño, Karlo L. ; Faustino-Eslava, Decibel V. ; Marquez, Edanjarlo J. ; Ramos, Noelynna T. ; Payot, Betchaida D. ; Guotana, Juan Miguel R. ; Gabo-Ratio, Jillian Aira S. ; Armada, Leo T. ; Padrones, Jenielyn T. ; Ishida, Keisuke ; Suzuki, Shigeyuki. / Slab rollback and microcontinent subduction in the evolution of the Zambales Ophiolite Complex (Philippines) : A review. In: Geoscience Frontiers. 2019.
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abstract = "New radiolarian ages show that the island arc-related Acoje block of the Zambales Ophiolite Complex is possibly of Late Jurassic to Early Cretaceous age. Radiometric dating of its plutonic and volcanic-hypabyssal rocks yielded middle Eocene ages. On the other hand, the paleontological dating of the sedimentary carapace of the transitional mid-ocean ridge – island arc affiliated Coto block of the ophiolite complex, together with isotopic age datings of its dikes and mafic cumulate rocks, also yielded Eocene ages. This offers the possibility that the Zambales Ophiolite Complex could have: (1) evolved from a Mesozoic arc (Acoje block) that split to form a Cenozoic back-arc basin (Coto block), (2) through faulting, structurally juxtaposed a Mesozoic oceanic crust with a younger Cenozoic lithospheric fragment or (3) through the interplay of slab rollback, slab break-off and, at a later time, collision with a microcontinent fragment, caused the formation of an island arc-related ophiolite block (Acoje) that migrated trench-ward resulting into the generation of a back-arc basin (Coto block) with a limited subduction signature. This Meso-Cenozoic ophiolite complex is compared with the other oceanic lithosphere fragments along the western seaboard of the Philippines in the context of their evolution in terms of their recognized environments of generation.",
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