Volcanism in Response to Plate Flexure

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 alka...

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Published inScience (American Association for the Advancement of Science) Vol. 313; no. 5792; pp. 1426 - 1428
Main Authors Hirano, Naoto, Takahashi, Eiichi, Yamamoto, Junji, Abe, Natsue, Ingle, Stephanie P, Kaneoka, Ichiro, Hirata, Takafumi, Kimura, Jun, Ishii, Teruaki, Ogawa, Yujiro, Machida, Shiki, Suyehiro, Kiyoshi
Format Journal Article
LanguageEnglish
Published Washington, DC American Association for the Advancement of Science 08.09.2006
The American Association for the Advancement of Science
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Summary: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.
Bibliography:http://www.scienceonline.org/
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ISSN:0036-8075
1095-9203
DOI:10.1126/science.1128235