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437 (0,064s)

Výsledek výzkumu

Subcrustal lithosphere around the Saxothuringian-Moldanubian Suture Zone - a model derived from anisotropy of seismic wave velocities.

We have modelled the thickness and large-scale fabric of the subcrustal lithosphere from the variations of P-wave delay times and the shear-wave splitting observed at seismological observatories and four mobile stations in central E...

DC - Seismologie, vulkanologie a struktura Země

  • 2001
  • Jx
Výsledek výzkumu

Subcrustal Continental Lithosphere - trade-off between Seismic Anisotropy and Heterogenity.

Annotation not available...

DC - Seismologie, vulkanologie a struktura Země

  • 1993
  • D
Výsledek výzkumu

Subcrustal lithosphere of the Variscan foldbelt in Central Europe - a model derived from anisotropy of seismic wave velocities.

Annotation not available...

DC - Seismologie, vulkanologie a struktura Země

  • 1998
  • Jx
Výsledek výzkumu

Teleseismic P-residual study in the Italian region - inferences on large scale anisotropic structure of the subcrustal lithosphere.

Annotation not available...

DC - Seismologie, vulkanologie a struktura Země

  • 1998
  • Jx
Výsledek výzkumu

Mapping the lithosphere-asthenosphere boundary through changes in surface-wave anisotropy.

The alignment of olivine crystals is considered as the dominant source of seismic anisotropy in the subcrustal lithosphere and asthenosphere. Different components of large-scale anisotropy can be traced in depth distributions of the...

DC - Seismologie, vulkanologie a struktura Země

  • 2002
  • Jx
Výsledek výzkumu

Seismic anisotropy of the lithosphere around the Trans-European Suture Zone (TESZ) based on teleseismic body-wave data of the TOR experiment.

A passive teleseismic experiment, traversing the northern part of the Trans-European Suture Zone in Germany, Denmark and Sweden, recorded data for tomography of the upper mantle with a lateral resolution of few tens of kilometers as well as for a det...

DC - Seismologie, vulkanologie a struktura Země

  • 2002
  • Jx
Výsledek výzkumu

Seismic structure and location of a CO2 source in the upper mantle of the western Eger (Ohře) Rift, central Europe

P-SV conversions provide new insights into the lithosphere of the western Eger Rift, a presently active CO2 emanation area, Quaternary volcanic field, and earthquake swarm region in central Europe. Gas and isotope mapping of free gas phases ...

DC - Seismologie, vulkanologie a struktura Země

  • 2005
  • Jx
Výsledek výzkumu

Subcrustal CO2 flux measurement in the Hranice hydrothermal Karst, methodology and first results

Hranice hydrothermal Karst is developed in the sequence of Paleozoic limestones as a result of deep influx of thermal water charged with subcrustal carbon dioxide (CO2). Flux CO2 (g.m-2.d-1) was measured in the soil and cave. The average soi...

DD - Geochemie

  • 2012
  • Jx
Výsledek výzkumu

Lithospheric stress tensor from gravity and lithospheric structure models

In this study we investigate the lithospheric stresses computed from the gravity and lithospheric structure models. The functional relation between the lithospheric stress tensor and the gravity field parameters is formulat...

Earth and related environmental sciences

  • 2017
  • Jimp
  • Odkaz
Výsledek výzkumu

Seismic anisotropy - a key to resolve fabrics of mantle lithosphere of Fennoscandia

We model lithosphere thickness and anisotropic structure in one of the oldest continental regions on the planet - the Fennoscandian Shield. Anisotropic domains of the mantle lithosphere retaining a fossil olivine fabric indicate an ...

DC - Seismologie, vulkanologie a struktura Země

  • 2008
  • Jx
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