ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2006
    Keywords: Fault zone ; NAFZ ; Stress ; Coulomb ; Structural geology ; JGR ; Cagatay ; Goeruer ; Gorur ; Marmara ; Sea ; multibeam ; bathymetry ; fault ; bends ; seafloor ; rupture ; Izmit ; earthquake ; 3045 ; Marine ; Geology ; and ; Geophysics: ; Seafloor ; morphology, ; geology, ; and ; geophysics ; 7221 ; Seismology: ; Paleoseismology ; (8036) ; 7250 ; Transform ; faults ; 8111 ; Tectonophysics: ; Continental ; tectonics: ; strike-slip ; and ; transform ; 8150 ; Plate ; boundary: ; general ; (3040)
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    In:  Eos Trans. AGU, Basel, Elsevier Science Publishers, vol. 87, no. 17, pp. 165,168, pp. 1025, (ISSN: 1340-4202)
    Publication Date: 2006
    Keywords: Sea seismics, ; Earthquake, ; Banda, ; Aceh, ; Nias, ; Project report/description ; Fluh ; Gadicke ; 3045 ; Marine ; Geology ; and ; Geophysics: ; Seafloor ; morphology, ; geology, ; and ; geophysics ; 3060 ; Subduction ; zone ; processes ; 7230 ; Seismology: ; Seismicity ; and ; tectonics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    In:  J. Geophys. Res., Hannover, Conseil de l'Europe, vol. 107, no. B10, pp. ETG 10-1 to ETG 10-10, pp. 2241, (ISSN: 1340-4202)
    Publication Date: 2002
    Keywords: Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Inelastic ; Rheology ; Subduction zone ; 7209 ; Seismology: ; Earthquake ; dynamics ; and ; mechanics ; 3040 ; Marine ; Geology ; and ; Geophysics: ; Plate ; tectonics ; (8150, ; 8155, ; 8157, ; 8158) ; 8150 ; Tectonophysics: ; Plate ; boundary--general ; (3040) ; 7230 ; Seismology: ; Seismicity ; and ; seismotectonics ; JGR
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    In:  Geophys. Res. Lett., Hannover, Conseil de l'Europe, vol. 32, no. 4, pp. 1886-1887, pp. L04301, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: Earthquake ; Seismicity ; red ; silent ; Earthquake asperities ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Global Positioning System ; Geodesy ; Subduction zone ; Canada ; GRL ; 1242 ; Geodesy ; and ; Gravity: ; Seismic ; cycle ; related ; deformations ; (6924, ; 7209, ; 7223, ; 7230) ; 1207 ; Transient ; deformation ; (6924, ; 7230, ; 7240) ; 1240 ; Satellite ; geodesy: ; results ; (6929, ; 7215, ; 7230, ; 7240) ; 3060 ; Marine ; Geology ; and ; Geophysics: ; Subduction ; zone ; processes ; (1031, ; 3613, ; 8170, ; 8413) ; 7215 ; Seismology: ; Earthquake ; source ; observations ; (1240)
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    In:  J. Geophys. Res., Amsterdam, Schweizerbart'sche Verlagsbuchhandlung, vol. 107, no. B10, pp. ECV 6-1-ECV 6-17, pp. 2223, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 2002
    Description: We use laboratory experiments and numerical models to quantify the effects of dike interaction on the focusing of magma as it ascends in the upper mantle. Laboratory experiments involve injecting buoyant fluid into the base of a tank filled with solidified gelatin. When we initiate two dikes parallel to each other, but separated by a horizontal distance x, they tend to merge as they ascend. This behavior is also predicted by numerical models of two-dimensional dikes. The key parameters that control the maximum horizontal separation x c over which dikes will intersect are dike driving pressures, dike head lengths L (i.e., the length over which driving pressure is large), and the difference between the principal stresses of the remote stress field. When the remote differential stress is small compared to the dike driving pressure, two dikes of equal driving pressure and length will intersect over distances of x c ? L. This distance decreases with increasing remote differential stress. We quantify the effects on magma transport from a broad lateral distribution of magma using numerical simulations of multiple-dike interaction. When the average dike spacing prior to interaction is within ?3 L and remote differential stresses are insignificant, dike interaction can focus magma over horizontal distances many times L but at least ?6 L. Dike interaction can focus magma in the asthenosphere beneath mid-ocean ridges for low mantle viscosities (?10 19 Pa s) and if dikes initiate with average separations of a few hundred meters, or less. Such focusing is predicted to grow dikes of increasing magma flux approaching lateral separations of a kilometer.
    Keywords: Fluids ; Plate tectonics ; ascent ; sheeted ; dykes ; Modelling ; JGR ; 8434 ; Volcanology: ; Magma ; migration ; 8145 ; Tectonophysics: ; Physics ; of ; magma ; and ; magma ; bodies ; 8120 ; Dynamics ; of ; lithosphere ; and ; mantle--general ; 3035 ; Marine ; Geology ; and ; Geophysics: ; Midocean ; ridge ; processes
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    In:  J. Geophys. Res., San Francisco, Schweizerbart'sche Verlagsbuchhandlung, vol. 110, no. B09410, pp. 205-218, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 2005
    Description: Theoretical and experimental studies indicate that when oceanic crust is hotter than about 800 C, variations in crustal thickness drive lower crustal flow. We investigate the nature of crustal flow beneath Iceland, where zero-age crust varies in thickness from under 20 km to over 40 km over a distance of 100 km and temperatures exceed 1000 C below depths of a few kilometers. We model the regional characteristics of crustal flow using the two-dimensional channel flow equation with depth-dependent viscosity. The model predicts the observed decay in crustal thickness contrasts between zero-age and off-axis crust on shore Iceland and development of a sharp Moho step as the plate moves away from the rift axis. These features become locked in place as plate cooling increases the viscosity. Observations are best matched by model predictions when the solidus viscosity is of order 10^18 Pa s, in agreement with viscosity estimates from deformation rates associated with deglaciation and plate boundary processes. Crustal flow acts to erase the crustal thickness memory of ridge-plume interaction, so that maps of Icelandic crustal thickness can be used neither to derive a detailed plume flux history nor to test in detail whether the Iceland Plume center is fixed relative to other hot spots. Crustal flow beneath Iceland is an unusually clear example of the kind of flow postulated to explain continental phenomena including exhumation of metamorphic core complexes and associated development of low-angle detachments within extensional terrains and sharp-edged plateau topography in major collisional belts
    Keywords: Rheology ; Plate tectonics ; GeodesyY ; ConvolutionE ; crustal ; flow ; Iceland ; viscosity ; 8137 ; Tectonophysics: ; Hotspots, ; large ; igneous ; provinces, ; and ; flood ; basalt ; volcanism ; 8120 ; Dynamics ; of ; lithosphere ; and ; mantle: ; general ; (1213) ; 3035 ; Marine ; Geology ; and ; Geophysics: ; Midocean ; ridge ; processes ; 8011 ; Structural ; Geology: ; Kinematics ; of ; crustal ; and ; mantle ; deformation ; 9325 ; Geographic ; Location: ; Atlantic ; Ocean
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    In:  Tectonics, Warszawa, Conseil de l'Europe, vol. 21, no. 5, pp. 10-1 to 10-17, pp. 1046, (ISSN: 1340-4202)
    Publication Date: 2002
    Keywords: Fault zone ; Greece ; 3025 ; Marine ; Geology ; and ; Geophysics: ; Marine ; seismics ; (0935) ; 8010 ; Structural ; Geology: ; Fractures ; and ; faults ; 8105 ; Tectonophysics: ; Continental ; margins ; and ; sedimentary ; basins ; 8107 ; Continental ; neotectonics ; 8123 ; Dynamics, ; seismotectonic
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2002
    Keywords: Structural geology ; rifting ; Fault zone ; Volcanology ; 8010 ; Structural ; Geology: ; Fractures ; and ; faults ; 8150 ; Tectonophysics: ; Plate ; boundary ; general ; (3040) ; 3035 ; Marine ; Geology ; and ; Geophysics: ; Midocean ; ridge ; processes ; 9325 ; Information ; Related ; to ; Geographic ; Region: ; Atlantic ; Ocean ; JGR ; Gljufura
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    In:  Geophys. Res. Lett., Oxford and Edinburgh, Blackwell Scientific Publications, vol. 29, no. 10, pp. 122-1 to 122-4, pp. 1484, (ISBN: 0534351875, 2nd edition)
    Publication Date: 2002
    Keywords: Earthquake ; Tsunami(s) ; Modelling ; GRL ; Hebert ; Schindele ; 3020 ; Marine ; Geology ; and ; Geophysics: ; Littoral ; processes ; 4255 ; Oceanography: ; General: ; Numerical ; modeling ; 4564 ; Physical: ; Tsunamis ; and ; storm ; surges ; 9355 ; Information ; Related ; to ; Geographic ; Region: ; Pacific ; Ocean ; SRICHWALSKI
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    In:  Geophys. Res. Lett., Minsk, Polish Geothermal Association, vol. 33, no. 3, pp. 684-692, pp. L03313, (ISSN: 1340-4202)
    Publication Date: 2006
    Keywords: Earthquake ; Fracture ; Source ; Subduction zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; tide ; gauges ; Global Positioning System ; Seismology ; GRL ; 3060 ; Marine ; Geology ; and ; Geophysics: ; Subduction ; zone ; processes ; (1031, ; 3613, ; 8170, ; 8413) ; 4564 ; Oceanography: ; Physical: ; Tsunamis ; and ; storm ; surges ; 7215 ; Seismology: ; Earthquake ; source ; observations ; (1240) ; 7240 ; Subduction ; zones ; (1207, ; 1219, ; 1240)
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...