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

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F11%3A00348396" target="_blank" >RIV/67985530:_____/11:00348396 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1007/s00531-010-0543-0" target="_blank" >http://dx.doi.org/10.1007/s00531-010-0543-0</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00531-010-0543-0" target="_blank" >10.1007/s00531-010-0543-0</a>

Result language
angličtina
Original language name
Recent plumbing system of the Krakatau volcano revealed by teleseismic earthquake distribution
Original language 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 adeep-rooted fault zone cutting the Sunda Strait in the SSW-NNE direction.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Project
<a href="/en/project/ME09011" target="_blank" >ME09011: Subduction Factory: Earthquake Production and Magma Emplacement</a><br>
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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