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72 (0,106s) •

Project

Prograde metamorphism, crustal thickening and lower crustal flow new concept of building of crustal root in Variscan orogen (GA13-16315S)

Mechanisms related to crustal thickening and lower crustal redistribution in the Bohemian Massif will be investigated by answering following questions: 1) How can be discriminated crustal thickening from subduction metamorp...

DB - Geologie a mineralogie

  • 2013 - 2016
    • •
  • 7 935 tis. Kč
    • •
  • 7 935 tis. Kč
    • •
  • GA ČR
Project

Crustal growth and construction of continental crust exemplified by Central Asian Orogenic Belt (GAP210/12/2205)

The project deals with revision of current models of crustal growth and crustal construction mechanisms, using the Mongolian and Chinese tract of the Central Asian of continental growth in the CAOB? 2) Was it crustal growth...

DB - Geologie a mineralogie

  • 2012 - 2015
    • •
  • 7 105 tis. Kč
    • •
  • 7 105 tis. Kč
    • •
  • GA ČR
Project

The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust (LK11202)

) Estimation of net crustal growth vs. recycling of preexistent crustal material zonationof individual crustal domains such as fossil andean or japan type arc......

DB - Geologie a mineralogie

  • 2012 - 2016
    • •
  • 25 736 tis. Kč
    • •
  • 23 415 tis. Kč
    • •
  • MŠMT
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 to application of simplistic 1D velocity models. The aim of the project is ...

DC - Seismologie, vulkanologie a struktura Země

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

Seismic and rheological features of the lower crustal rocks and their contribution to the anizotropy of the litosphere (GP205/02/D139)

This project aims to calibrate seismic data obtained from the lower-crustal rocks against strain. The Earth´s lower crust represents the weakest part of the lithosphere which is easily deformed and thus plays a key role during the orogenesis...

DB - Geologie a mineralogie

  • 2002 - 2005
    • •
  • 1 220 tis. Kč
    • •
  • 676 tis. Kč
    • •
  • GA ČR
Project

Crustal structure in the seismoactive region of the West Bohemia (GAP210/10/2063)

Knowledge of a detailed crustal structure is essential for all advanced studies of seismicity and focal parameters of microearthquakes in the West Bohemia/Vogtland region. Although the geological structure is complicated in this area, with v...

DC - Seismologie, vulkanologie a struktura Země

  • 2010 - 2012
    • •
  • 1 369 tis. Kč
    • •
  • 1 369 tis. Kč
    • •
  • GA ČR
Project

Internal strain fabric and rheology of orogenic peridotites and surrounding crustal rocks (GA205/09/0539)

studies carried out on a high-temperature crustal rocks that surround upper mantle andpetrological investigation of lower crustal rocks is proposed in localities that have and surrounding crustal rocks in order to evaluate...

DB - Geologie a mineralogie

  • 2009 - 2012
    • •
  • 2 954 tis. Kč
    • •
  • 2 954 tis. Kč
    • •
  • GA ČR
Project

Dynamics of crustal fluids in the western part of the Bohemian Massif as a probe of the stress changes (IAA300120905)

Analysis of seismogenic stress variations and their effect to crustal fluids is often complicated due to the singular and irregular occurrence of earthquakes and unknown origin of the associated stress changes, which lie deep in the crust of...

DC - Seismologie, vulkanologie a struktura Země

  • 2009 - 2012
    • •
  • 2 495 tis. Kč
    • •
  • 2 495 tis. Kč
    • •
  • AV ČR
Project

Geodetic Investigations of Recent Crustal Movements in the Seismoactive Area Western-Bohemia-Vogtland. (GA205/94/1208)

DC - Seismologie, vulkanologie a struktura Země

  • 1994 - 1996
    • •
  • 215 tis. Kč
    • •
  • 295 tis. Kč
    • •
  • GA ČR
Project

Relation of extrusion and horizontal flow of lower crust to the origin of the lower crustal wedge along eastern margin of Bohemian massive (GA205/04/2065)

Large scale wedge structure formed by lower crustal rocks as granulites, eclogites and migmatites has been identified in the Moldanubian zone along the eastern margin of the Bohemia Massif. This lower crustal wedge structure has a c...

DB - Geologie a mineralogie

  • 2004 - 2006
    • •
  • 810 tis. Kč
    • •
  • 810 tis. Kč
    • •
  • GA ČR
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