Tomographic Images of Klyuchevskoy Volcano P-Wave Velocity

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dc.contributor Eichelberger J.
dc.contributor Gordeev E.
dc.contributor Izbekov P.
dc.contributor Kasahara M.
dc.contributor Lees J.
dc.contributor.author Lees J.
dc.contributor.author Symons N.
dc.contributor.author Chubarova O.
dc.contributor.author Gorelchik V.
dc.contributor.author Ozerov A.
dc.date.accessioned 2019-09-03T12:46:59Z
dc.date.available 2019-09-03T12:46:59Z
dc.date.issued 2007
dc.identifier http://repo.kscnet.ru/3498/
dc.identifier http://repo.kscnet.ru/3498/1/2007_Lees_et_al_Kluch.pdf
dc.identifier https://agupubs.onlinelibrary.wiley.com/doi/10.1029/172GM21
dc.identifier.citation Lees J., Symons N., Chubarova O., Gorelchik V., Ozerov A. (2007) Tomographic Images of Klyuchevskoy Volcano P-Wave Velocity // Volcanism and Subduction: The Kamchatka Region. Geophysical Monograph Series. / Eichelberger J., Gordeev E., Izbekov P., Kasahara M., Lees J. eds. Washington, D. C.: American Geophysical Union Vol. 172. pp. 293-302.
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/6214
dc.description.abstract Three-dimensional structural images of the P-wave velocity below the edifice of the great Klyuchevskoy group of volcanoes in central Kamchatka are derived via tomographic inversion. The structures show a distinct low velocity feature extending from around 20 km depth to 35 km depth, indicating evidence of magma ponding near the Moho discontinuity. The extensive low velocity feature represents, at least to some degree, the source of the large volume of magma currently erupting at the surface near the Klyuchevskoy group.
dc.language.iso en
dc.publisher American Geophysical Union
dc.subject 38.01.77 Методы исследования и моделирования. Математические и кибернетические методы в геологии
dc.subject 38.37.25 Вулканология
dc.subject Ключевской
dc.title Tomographic Images of Klyuchevskoy Volcano P-Wave Velocity
dc.type Раздел книги


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