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836 (0,089s)

Project

Physical processes in an earthquake source from micro- to macro-scale (GAP210/12/1491)

The aim of the project is to study earthquake source processes at various scales in order to find links between micro- and macro-seismicity and to understand what we can learn from studies of acoustic emissions and micro-se...

DC - Seismologie, vulkanologie a struktura Země

  • 2012 - 2016
  • 6 558 tis. Kč
  • 6 558 tis. Kč
  • GA ČR
Project

CRUSTAL STRUCTURE DETERMINED FROM WAVEFORMS OF LOCAL MICRO-EARTHQUAKES (GA13-08971S)

Knowledge of a detailed crustal structure is essential for all advanced studies of seismicity and focal parameters of micro-earthquakes. In many cases it is confined structure from waveforms of local micro-earthquakes

DC - Seismologie, vulkanologie a struktura Země

  • 2013 - 2015
  • 3 151 tis. Kč
  • 3 151 tis. Kč
  • GA ČR
Project

NEW INTEGRATED KNOWLEDGE BASED APPROACHES TO THE PROTECTION OF CULTURAL HERITAGE FROM EARTHQUAKE-INDUCED RISK (7E10053)

The project tackles the problem of earthquake-impact on Cultural Heritage assets starting from basic consideration that efficient protection, with substantial conditions. At the project start, earthquake-induced failure mechanisms, ...

JN - Stavebnictví

  • 2010 - 2012
  • 1 491 tis. Kč
  • 1 491 tis. Kč
  • MŠMT
Project

Seismic Processes and Parameters of the Upper crust medium in the West Bohemian earthqueke swarm region (GA205/96/0974)

of swarm-like nature. The seismic energy between two major earthquake swarms is released in the form of large number of micro-earthquakes, the hypocentres beingSeismological research in the region of West Bohemian eart...

DC - Seismologie, vulkanologie a struktura Země

  • 1996 - 1998
  • 3 022 tis. Kč
  • 1 726 tis. Kč
  • GA ČR
Project

NAtural Seismicity as a Prospecting and MONitoring tool for geothermal energy extraction (TO01000198)

geothermal sources and micro-earthquake activityObjectives a) to create new knowledge of the physical processes that cause earthquakes with special emphasis on the role of fluids, geothermal operations and tectonic plate m...

Other natural sciences

  • 2021 - 2024
  • 38 283 tis. Kč
  • 27 836 tis. Kč
  • TA ČR
Project

Time-development analyses of microdisplacements monitored in the collision zone between African and Euro-Asian plates (GA205/09/2024)

and short-term impulses. Micro-displacements occured during so call impulses can be parallel with registered local earthquakes. The goal of the project is continuation in monitoring of micro-displacements and their time-de...

DB - Geologie a mineralogie

  • 2009 - 2011
  • 3 858 tis. Kč
  • 3 858 tis. Kč
  • GA ČR
Project

3-D monitoring of micro-movements in the effective collision zone between African and Euro-Asian plates (GA205/06/1828)

3D monitoring of micro-movements in the effective collision zone between African and Euro-Asian plates Monitoring of micro-movements on tectonic fault structures provides essential data for solution of mechanical questions concernin...

DB - Geologie a mineralogie

  • 2006 - 2008
  • 3 388 tis. Kč
  • 3 388 tis. Kč
  • GA ČR
Project

European network on seismic risk, vulnerability and earthquake scenarios (OK 345)

Risk, Vulnerability and Earthquake Scenarios" (ENSeRVES) is a part of the 4th Frame andapplications in (a) earthquake hazard assessment, (b) earthquake vulnerability of structures and of their ground formations, (c) seismi...

DC - Seismologie, vulkanologie a struktura Země

  • 1998 - 2001
  • 1 729 tis. Kč
  • 1 323 tis. Kč
  • MŠMT
Project

Understanding earthquakes in Western Greece (ME 354)

Earthquake prediction fails because deep processes do not allow direct physical measurements. The only way how to reduce damaging effects of future earthquakes is to understand well recorded past events by means of their theoretical...

DC - Seismologie, vulkanologie a struktura Země

  • 2000 - 2001
  • 530 tis. Kč
  • 230 tis. Kč
  • MŠMT
Project

Dynamics of subducting slabs and origin of deep-focus earthquakes (LUAUS23233)

Earthquakes occur mainly in subduction zones. While the mechanism of shallow earthquakes (up to 70 km) is identified as frictional faulting at the contact of subducting and overriding plates, the origin of deep-focus earthquakes...

Geology

  • 2023 - 2026
  • 6 131 tis. Kč
  • 6 131 tis. Kč
  • MŠMT
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