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Zambales Ophiolite Complex information


Zambales Ophiolite
Stratigraphic range: Late Jurassic to Middle Eocene~161.5–40.4 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeGeological formation
Unit ofZambales Range
UnderliesConstitutes the basement of Zambales
OverliesBalog-Balog Diorite and Aksitero Formation
Lithology
PrimaryPeridotite, gabbro, diabasic dike complex, diorite, pillow basalt, pelagic limestone, sandstone, mudstone
Location
RegionCentral Luzon
CountryPhilippines
Type section
Named forZambales
Named byBureau of Mines and Geosciences
Year defined1981

The Zambales Ophiolite Complex (also called Zambales Ophiolite) is a large, well-preserved exposure of oceanic crust located in the western portion of Luzon Island, Philippines.[1] It is considered one of the best-preserved and most studied ophiolites, offering valuable insights into the formation and evolution of oceanic crust and the processes involved in plate tectonics.

  1. ^ Salapare, Ricky C.; Dimalanta, Carla B.; Ramos, Noelynna T.; Manalo, Pearlyn C.; Faustino-Eslava, Decibel V.; Queaño, Karlo L.; Yumul, Graciano P. Jr. (June 2015). "Upper crustal structure beneath the Zambales Ophiolite Complex, Luzon, Philippines inferred from integrated gravity, magnetic and geological data". Geophysical Journal International. 201 (3): 1522–1533. doi:10.1093/gji/ggv094.

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