Zobrazeno 1 - 10 of 59 pro vyhledávání: '"Günter Bock"'
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The M w 3.1–4.7 earthquakes in the southern Baltic Sea and adjacent areas in 2000, 2001 and 2004
Autor: K. Wylegalla, Gottfried Grünthal, Günter Bock, Rainer Kind, Dietrich Stromeyer, Rutger Wahlström, Xiaohui Yuan
Publikováno v: Journal of Seismology
The area south and east of the Baltic Sea has very minor seismic activity. However, occasional events occur as illustrated by four events in recent years, which are analysed in this study: near Wittenburg, Germany, on May 19, 2000, M w = 3.1, near Ro
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8acf2ac57a9eea91fd88e0af70a36ad3
https://doi.org/10.1007/s10950-008-9096-0
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6
The 1985/86 Western Bohemia earthquakes: Modelling source parameters with synthetic seismograms
Autor: Gottfried Grünthal, K. Wylegalla, Günter Bock
Publikováno v: Tectonophysics. 261:139-146
A major swarm of microearthquakes (main shock: M L = 4.6) occurred in December 1985 and January 1986 in the western Bohemia region (50.2°N, 12.4°E). Here, we revisit the 1985/86 series by modelling some pronounced features of the observed P wavefor
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::75a50eedd17ae60a24195eccde6e1293
https://doi.org/10.1016/0040-1951(96)00062-5
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8
Upper Mantle Structure Beneath the Eifel from Receiver Functions
Autor: Martin Budweg, Günter Bock, Michael E Weber
Publikováno v: Mantle Plumes ISBN: 9783540680451
Mantle Plumes-A Multidisciplinary Approach
The average Moho depth in the Eifel is approximately 30 km, thinning to ca. 28 km under the Eifel volcanic fields. Receiver function (RF) images suggest the existence of a low velocity zone at about 60 to 90 km depth underneath the West Eifel. This o
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::84a63c2f81808657ec85385d42f81ce6
https://doi.org/10.1007/978-3-540-68046-8_13
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9
The Eifel Plume - imaged with converted seismic waves
Autor: Martin Budweg, Günter Bock, Michael E Weber
Publikováno v: Geophysical Journal International
Receiver functions (RF) are used to investigate the upper mantle structure beneath the Eifel, the youngest volcanic area of Central Europe. Data from 96 teleseismic events recorded by 242 seismological stations from permanent and a temporary network
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b6ceac197530a05d2ed5bd15ee410822
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:234597
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10
Boundary-layer mantle flow under the Dead Sea transform fault inferred from seismic anisotropy
Autor: Georg Rümpker, Trond Ryberg, Günter Bock, null Desert Seismology Group
Publikováno v: Nature
Lithospheric-scale transform faults play an important role in the dynamics of global plate motion. Near-surface deformation fields for such faults are relatively well documented by satellite geodesy, strain measurements and earthquake source studies,
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fa4c73dba9ba48616d1df9cf79e5555a
https://gfzpublic.gfz-potsdam.de/pubman/item/item_229793_1/component/file_229792/4007.pdf
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