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106 (0,087s) •

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
Project

Information net for fast access to data about strong mevement and makroseismic intensities of improtant earthquakes in Greece.(S.M.INT) (ME 694)

Goal of project is developingt net for fast access to informations about earthquakes in Greece (using web pages)....

JA - Elektronika a optoelektronika, elektrotechnika

  • 2003 - 2005
    • •
  • 1 007 tis. Kč
    • •
  • 486 tis. Kč
    • •
  • MŠMT
Project

Earthquake migration patterns A key to understand the triggering mechanisms (GA20-26018S)

Earthquake hypocenter migration is the most characteristic pattern which involve creep, fluid migration or similar. While interactions among earthquakes can in seismic datasets of earthquake swarms and induced seismicity, m...

Geology

  • 2020 - 2022
    • •
  • 2 145 tis. Kč
    • •
  • 2 145 tis. Kč
    • •
  • GA ČR
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 physical processes leading to large earthquakes. The project will focus on: (1) studying physical properties such as seismic anisotropy of a material at the <...

DC - Seismologie, vulkanologie a struktura Země

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

Physical processes related to swarm-like seismicity on the plate boundary in South Iceland and intraplate earthquake swarms in West-Bohemia/Vogtland (GA18-05053S)

Earthquake swarms are a specific type of seismicity which occurs in diverse can help us to understand the physical nature of even stronger earthquakes seismicity in SW Iceland and its comparison to earthquake swarms in West...

Geology

  • 2018 - 2021
    • •
  • 10 514 tis. Kč
    • •
  • 9 612 tis. Kč
    • •
  • GA ČR
Project

Multiscale spatial-temporal complexity of tectonic earthquake sources (GA14-04372S)

The complexity of tectonic earthquake sources is recognized both in spatial earthquakes (Mw 6-9), utilizing various data sets (including seismic and gravity the multi-scale character of the earthquake source. The proposed a...

DC - Seismologie, vulkanologie a struktura Země

  • 2014 - 2016
    • •
  • 3 947 tis. Kč
    • •
  • 3 947 tis. Kč
    • •
  • GA ČR
Project

Earthquake swarms and their triggering mechanisms in diverse tectonic environments (Bohemian Massif, Mid-Atlantic Ridge, Western Alps) (GAP210/12/2336)

Earthquake swarms occur in various geological units. They have been studied of earthquake swarms instead of ordinary single events or mainshock-aftershock sequences. In our project, we will investigate the earthquake swarms...

DC - Seismologie, vulkanologie a struktura Země

  • 2012 - 2016
    • •
  • 11 775 tis. Kč
    • •
  • 11 775 tis. Kč
    • •
  • GA ČR
Project

Earthquake hazard for the Czech Republic corrected on local geology effects (GA205/05/2287)

Standard seismostatistic approach of the earthquake hazard will be extended for corrections on local geology effects that often significantly change amplitude and frequency contents of seismic waves and in this way their impacts to building ...

DC - Seismologie, vulkanologie a struktura Země

  • 2005 - 2007
    • •
  • 1 237 tis. Kč
    • •
  • 1 237 tis. Kč
    • •
  • GA ČR
  • 1 - 10 out of 106