Ontong Java Plateau
The Ontong Java Plateau (OJP) is a huge oceanic plateau located in the south-west Pacific Ocean, north of the Solomon Islands. The OJP was emplaced c. 120 Ma with a much smaller volcanic event c. 90 Ma. Two other south-west Pacific plateaus, Manihiki and Hikurangi, now separated from the OJP by Cretaceous ocean basins, are of similar age and composition and probably formed as a single plateau and a contiguous large igneous province together with the OJP.[1] When emplaced this Ontong Java-Manihiki-Hikurangi plateau covered 1% of Earth's surface and represented a volume of 1,000,000 km3 (240,000 cu mi) of basaltic magma.[2] This "Onotong Java event", first proposed in 1991, represents the largest volcanic event of the past 200 million years, with a magma emplacement rate estimated at up to 22 km3 (5.3 cu mi)/year over three million years, several times larger than the Deccan Traps.[3] The smooth surface of the OJP is punctuated by seamounts such as the Ontong Java Atoll, the largest atoll in the world.[4]
Geological setting
The OJP covers 1,500,000 km2 (580,000 sq mi), roughly the size of Alaska. It reaches up to 1,700 m (5,600 ft) below sea level but has an average depth closer to 2–3 km (1.2–1.9 mi). It is bounded by Lyra Basin to the north-west, East Mariana Basin to the north, Nauru Basin to the north-east, and the Ellice Basin to the south-east. The OJP has collided with the Solomon Islands island arc and now lies on the inactive Vitiaz Trench and the Pacific-Australian plate boundary.[4]
The high plateau, with a crustal thickness estimated to at least 25 km (16 mi) but probably closer to 36 km (22 mi), has a volume of more than 5,000,000 km3 (1,200,000 cu mi). The maximum extent of the event can, however, be much larger since lavas in several surrounding basins are closely related to the OJP event and probably represent dike swarms associated with the emplacement of the OJP.[4]
Tectonic evolution
OJP formed quickly over a mantle plume head, most likely the then newly-formed Louisville hotspot, followed by limited volcanism for at least 30 million years. The extant seamounts of the Louisville seamount chain started to form 70 Ma and have a different isotopic composition, and therefore a shift in intensity and magma supply in the plume must have occurred before that.[5]
The early, short-duration eruptions of OJP coincide with the global Early Aptian oceanic anoxic event (known as OAE1a or the Selli Event, 125.0–124.6 Ma) that lead to the deposition of black shales during the interval 124–122 Ma. Additionally, isotopic records of seawater in sediments have been associated with the 90 Ma OJP submarine eruptions.[6]
About 80% of the OJP is being subducted beneath the Solomon Islands. Only the uppermost 7 km of the crust is preserved on the Australian Plate.[7] This collision has lifted some of the OJP above sea level on the islands of Makira, Malaita, and the northern half of Santa Isabel, and the smaller islands of Ramos and Ulawa.
References
Notes
- ^ Taylor 2006, Abstract
- ^ Worthington et al. 2006, Introduction, pp. 685–686
- ^ Tarduno et al. 1991, p. 401
- ^ a b c Neal et al. 1993, Physical features and gross structure of the OJP, pp. 184–187
- ^ Mahoney et al. 1993, Abstract
- ^ Tejada et al. 2009, Abstract; Introduction, pp. 855–856
- ^ Mann & taira 2004, Abstract
Sources
- Tejada, M. L. G.; Suzuki, K.; Kuroda, J.; Coccioni, R.; Mahoney, J. J.; Ohkouchi, N.; Sakamoto, T.; Tatsumi, Y. (2009). "Ontong Java Plateau eruption as a trigger for the early Aptian oceanic anoxic event" (PDF). Geology. 37 (9): 855–858. doi:10.1130/G25763A.1. Retrieved 17 December 2016.
{{cite journal}}: Invalid|ref=harv(help) - Mahoney, J. J.; Storey, M.; Duncan, R. A.; Spencer, K. J.; Pringle, M. (1993). "Geochemistry and age of the Ontong Java Plateau" (PDF). The Mesozoic Pacific: geology, tectonics, and volcanism. Geophys. Monogr. Ser. Vol. 77. Washington, D. C.: AGU. pp. 233–261. Bibcode:1993GMS....77..233M. doi:10.1029/GM077p0233. Retrieved 17 December 2016.
{{cite book}}: Invalid|ref=harv(help) - Mann, P.; Taira, A. (2004). "Global tectonic significance of the Solomon Islands and Ontong Java Plateau convergent zone" (PDF). Tectonophysics. 389 (3): 137–190. doi:10.1016/j.tecto.2003.10.024. Retrieved 18 December 2016.
{{cite journal}}: Invalid|ref=harv(help) - Neal, C. R.; Mahoney, J. J.; Kroenke, L. W.; Duncan, R. A.; Petterson, M. G. (1997). "The Ontong Java Plateau" (PDF). In Mahoney, J. J.; Coffin, F. (eds.). Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. Geophys. Monogr. Ser. Vol. 100. Washington D.C.: AGU. pp. 183–216. Bibcode:1997GMS...100..183N. doi:10.1029/GM100p0183. Retrieved 17 December 2016.
{{cite book}}: Invalid|ref=harv(help) - Tarduno, J. A.; Mayer, H.; Winterer, E. L.; Sliter, W. V.; Kroenke, L.; Mahoney, J. J.; Leckie, M.; Musgrave, R.; Storey, M. (1991). "Rapid formation of Ontong Java Plateau by Aptian mantle plume volcanism" (PDF). Science. 254 (5030): 399–403. Bibcode:1991Sci...254..399T. doi:10.1126/science.254.5030.399. Retrieved 17 December 2016.
{{cite journal}}: Invalid|ref=harv(help) - Taylor, Brian (31 January 2006). "The single largest oceanic plateau: Ontong Java-Manihiki-Hikurangi" (PDF). Earth and Planetary Science Letters. 241 (3–4): 372–380. Bibcode:2006E&PSL.241..372T. doi:10.1016/j.epsl.2005.11.049. Retrieved 17 December 2016.
{{cite journal}}: External link in|lay-url=|ref=harv(help); Unknown parameter|lay-date=ignored (help); Unknown parameter|lay-url=ignored (help) - Worthington, Tim J.; Hekinian, Roger; Stoffers, Peter; Kuhn, Thomas; Hauff, Folkmar (30 May 2006). "Osbourn Trough: Structure, geochemistry and implications of a mid-Cretaceous paleospreading ridge in the South Pacific" (PDF). Earth and Planetary Science Letters. 245 (3–4): 685–701. Bibcode:2006E&PSL.245..685W. doi:10.1016/j.epsl.2006.03.018. Retrieved 17 December 2016.
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Further reading
- Fitton, J. G.; Mahoney, J. J.; Wallace, P. J.; Saunders, A. D. (2004). "Origin & Evolution of the Ontong Java Plateau: introduction" (PDF). Geological Society, London, Special Publications. 229. doi:10.1144/GSL.SP.2004.229.01.01. ISBN 978-1-86239-157-4. Retrieved 17 December 2016.
{{cite journal}}: Invalid|ref=harv(help)(Ocean Drilling Program: Volume 192 Scientific Results)
