Ontong Java Plateau
The Ontong Java Plateau (OJP) is a huge oceanic plateau in the southwestern Pacific Ocean, north of the Solomon Islands. The OJP was formed around 120 million years ago. When eruption of lava ended, the Ontong plateau covered 1% of Earth's surface. It had a volume of 80 million km3 (19 million cu mi) of basaltic magma.
This Ontong Java event was the largest volcanic event of the past 200 million years. Its magma production was several times larger than the Deccan Traps. The smooth surface of the OJP is punctuated by seamounts such as the Ontong Java Atoll, one of the largest atolls in the world.
References
- ↑ Taylor 2006, Abstract
- ↑ Rizo 2016
- ↑ Tarduno et al. 1991, p. 401
- ↑ Neal et al. 1993, Physical features and gross structure of the OJP, pp. 184–187
- ↑ Neal, Clive R.; Mahoney, John J.; Kroenke, Loren W.; Duncan, Robert A.; Petterson, Michael G. (2013-03-18), "The Ontong Java Plateau", Large Igneous Provinces: continental, oceanic, and planetary flood volcanism, American Geophysical Union, pp. 183–216, doi:10.1029/gm100p0183, ISBN 978-1-118-66434-6
{{citation}}: CS1 maint: work parameter with ISBN (link)
Sources
- 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. ISBN 978-0-87590-036-0. Retrieved 17 December 2016.
{{cite book}}:|journal=ignored (help) - Mann, P.; Taira, A. (2004). "Global tectonic significance of the Solomon Islands and Ontong Java Plateau convergent zone". Tectonophysics. 389 (3): 137–190. Bibcode:2004Tectp.389..137M. doi:10.1016/j.tecto.2003.10.024. Retrieved 18 December 2016.
- 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. ISBN 9781118664346. Archived from the original (PDF) on 1 January 2017. Retrieved 17 December 2016.
{{cite book}}:|journal=ignored (help) - Rizo, H. (September 2016). "September 2016 LIP of the Month: Phanerozoic Large Igneous Provinces sample remnants of early differentiation events on Earth". Large Igneous Provinces Commission. Retrieved 14 April 2017.
- 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. PMID 17742226. S2CID 7627426. Retrieved 17 December 2016.
- Taylor, Brian (31 January 2006). "The single largest oceanic plateau: Ontong Java-Manihiki-Hikurangi". Earth and Planetary Science Letters. 241 (3–4): 372–380. Bibcode:2006E&PSL.241..372T. doi:10.1016/j.epsl.2005.11.049.
- "February 2006 LIP of the Month". Large Igneous Provinces Commission. 6 February 2006.
- 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". Geology. 37 (9): 855–858. Bibcode:2009Geo....37..855T. doi:10.1130/G25763A.1. Retrieved 17 December 2016.