Volcanism in Response to Plate Flexure
Hirano, N., Takahashi, E., Yamamoto, J., Abe, N., Ingle, S.P., Kaneoka, I., Hirata, T., Kimura, J., Ishii, T., Ogawa, Y., Machida, S. and Suyehiro, K. (2006) Volcanism in Response to Plate Flexure. Science, 313, (5792), 1426-1428. (doi:10.1126/science.1128235).
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Volcanism on Earth is known to occur in three tectonic settings: divergent plate boundaries (such as mid-ocean ridges), convergent plate boundaries (such as island arcs), and hot spots. We report volcanism on the 135 million-year-old Pacific Plate not belonging to any of these categories. Small alkalic volcanoes form from small percent melts and originate in the asthenosphere, as implied by their trace element geochemistry and noble gas isotopic compositions. We propose that these small volcanoes erupt along lithospheric fractures in response to plate flexure during subduction. Minor extents of asthenospheric melting and the volcanoes' tectonic alignment and age progression in the direction opposite to that of plate motion provide evidence for the presence of a small percent melt in the asthenosphere
|Digital Object Identifier (DOI):||doi:10.1126/science.1128235|
|Subjects:||Q Science > QE Geology|
|Divisions:||University Structure - Pre August 2011 > School of Ocean & Earth Science (SOC/SOES)
|Date Deposited:||09 Oct 2007|
|Last Modified:||06 Aug 2015 02:39|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
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