About: Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution

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An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Spatial and temporal analysis of global seismological data 1964–2005 reveals a distinct teleseismic earthquake activity producing a columnar-like formation in the continental wedge between the Krakatau volcano at the surface and the subducting slab of the Indo-Australian plate. These earthquakes occur continuously in time, are in the body-wave magnitude range 4.5–5.3 and in the depth range 1–100 km. The Krakatau earthquake cluster is vertical and elongated in the azimuth N30 E, suggesting existence of a deep-rooted fault zone cutting the Sunda Strait in the SSW-NNE direction. Spatial and temporal analysis of global seismological data 1964–2005 reveals a distinct teleseismic earthquake activity producing a columnar-like formation in the continental wedge between the Krakatau volcano at the surface and the subducting slab of the Indo-Australian plate. These earthquakes occur continuously in time, are in the body-wave magnitude range 4.5–5.3 and in the depth range 1–100 km. The Krakatau earthquake cluster is vertical and elongated in the azimuth N30 E, suggesting existence of a deep-rooted fault zone cutting the Sunda Strait in the SSW-NNE direction. (en)
Title	Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution (en)
skos:prefLabel	Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution (en)
skos:notation	RIV/67985530:_____/11:00348396!RIV12-AV0-67985530
http://linked.open...avai/predkladatel	Geofyzikální ústav AV ČR, v. v. i.
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(ME09011), Z(AV0Z30120515)
http://linked.open...iv/cisloPeriodika	6
http://linked.open...vai/riv/dodaniDat	2012
http://linked.open...aciTvurceVysledku	Hanuš, Václav Špičák, Aleš Vaněk, Jiří
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Geofyzikální ústav AV ČR, v. v. i.
http://linked.open...dnocenehoVysledku	225910
http://linked.open...ai/riv/idVysledku	RIV/67985530:_____/11:00348396
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	subduction-related volcanoes; Krakatau; earthquake distribution; volcanic plumbing system (en)
http://linked.open.../riv/klicoveSlovo	Krakatau earthquake distribution subduction-related volcanoes volcanic plumbing system
http://linked.open...odStatuVydavatele	DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV	[D5D960461A1C]
http://linked.open...i/riv/nazevZdroje	International Journal of Earth Sciences
http://linked.open...in/vavai/riv/obor	DC
http://linked.open...ichTvurcuVysledku	3 (xsd:int)
http://linked.open...cetTvurcuVysledku	3 (xsd:int)
http://linked.open...vavai/riv/projekt	Subduction Factory: Earthquake Production and Magma Emplacement
http://linked.open...UplatneniVysledku	2011
http://linked.open...v/svazekPeriodika	100
http://linked.open...iv/tvurceVysledku	Vaněk, Jiří Hanuš, Václav Špičák, Aleš
http://linked.open...ain/vavai/riv/wos	000293776000011
http://linked.open...n/vavai/riv/zamer	Study of the internal structure and dynamics of the Earth
issn	1437-3254
number of pages	7 (xsd:int)
http://bibframe.org/vocab/doi	10.1007/s00531-010-0543-0
is http://linked.open...avai/riv/vysledek of	Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution

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