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36 (0,139s) •

Project

Geodynamic controls on continental rifting in Cenozoic central Europe insights from the Eger Rift, Bohemia (GA22-13980S)

Evolution of the Eger Rift (ER), the least known part of the European Cenozoic Rift System (ECRIS), will be studied by combining an evaluation of tectonic image of the tectonic structure of the rift will then serve...

Geology

  • 2022 - 2024
    • •
  • 7 574 tis. Kč
    • •
  • 7 574 tis. Kč
    • •
  • GA ČR
Project

Late Cenozoic to present tectonic activity of the western Eger Rift (GC16-10116J)

The project is focused to the assessment of Late cenozoic to present tectonic activity of the western Eger Rift, which is typified by Quaternary volcanism, present seismicity and CO2 degassing. The Mariánské Lázně Fault delimiting t...

DC - Seismologie, vulkanologie a struktura Země

  • 2016 - 2018
    • •
  • 6 604 tis. Kč
    • •
  • 6 345 tis. Kč
    • •
  • GA ČR
Project

Eger Rift - deep lithosphere structure, its origin and geodynamic development (GA205/07/1088)

Aim of this project is to study deep structure of the lithosphere-asthenosphere system beneath the Eger (Ohře) Rift in the north-western Bohemian Massif (central Europe) by means of seismic tomography and anisotropy. The target area...

DC - Seismologie, vulkanologie a struktura Země

  • 2007 - 2011
    • •
  • 1 974 tis. Kč
    • •
  • 1 974 tis. Kč
    • •
  • GA ČR
Project

Upper-crustal model of the Ohře Rift and its vicinity. (IAA300460602)

The region of the Ohře Rift in the northwestern part of the Bohemian Massif attracts attention of scientists due to the exceptional geological phenomena: contacts of geological units, significant faults, large granitic massifs, sedimentary b...

DC - Seismologie, vulkanologie a struktura Země

  • 2006 - 2010
    • •
  • 3 002 tis. Kč
    • •
  • 3 002 tis. Kč
    • •
  • AV ČR
Project

/Eger Rift) (IAA300130902)

Continental intraplate magmatism is commonly expressed in subvolcanic complexes, for which it is important to characterize the mantle sources. That necessitates distinguishing the effect upon mantle signature of fractional crystallization and assimil...

DD - Geochemie

  • 2009 - 2013
    • •
  • 4 004 tis. Kč
    • •
  • 4 004 tis. Kč
    • •
  • AV ČR
Project

Upper mantle beneath the neovolcanic zone of the Bohemian Massif xenoliths and their host basalts (GA205/09/1170)

of their lithospheric structures: the Ohře Rift and the Labe/Odra Zone. The proposed research...

DB - Geologie a mineralogie

  • 2009 - 2012
    • •
  • 3 139 tis. Kč
    • •
  • 2 879 tis. Kč
    • •
  • GA ČR
Project

Reference climate curve for the beginning of the Miocene Climatic Optimum in Central Europe (GA16-00800S)

The aim of the project is to assemble composite record of the evolution of continental environment in central Europe in period around the onset of Miocene Climatic Optimum from lacustrine sediments of the Most Basin in the Ohre (Eger) Ri...

DD - Geochemie

  • 2016 - 2018
    • •
  • 4 773 tis. Kč
    • •
  • 4 773 tis. Kč
    • •
  • GA ČR
Project

International Continental Scientific Drilling Program (ICDP) - membership fee of the Czech Republic (LA08036)

The aim of the project is to get funds to cover the annual membership fee of the Czech Republic in the International Continental Scientific Drilling Program (ICDP) between 2008-2012. Research associated with deep drilling is important in understandin...

DC - Seismologie, vulkanologie a struktura Země

  • 2008 - 2012
    • •
  • 3 300 tis. Kč
    • •
  • 3 300 tis. Kč
    • •
  • MŠMT
Project

Tectonic and volcanic controls on hydrothermal silicification in marginal zones of the Ohře Rift (IAA3013302)

Near-contact silicification along intrusive/volcanic bodies and large-volume silicification beneath sealing horizons are the two types of hydrothermal alteration with newly formed SiO2 in coarse clastics of the fill of the Ohře Rift graben (...

DB - Geologie a mineralogie

  • 2003 - 2006
    • •
  • 2 675 tis. Kč
    • •
  • 2 013 tis. Kč
    • •
  • AV ČR
Project

Did the West-Gondwana orogens form by inversion of long-lived rift domains? (GA18-24281S)

by ca. 200 My of rifting, and that inversion of the rift domain took place soon, or if the system is an inverted rift domain without major intervention of oceanic crust.......

Geology

  • 2018 - 2021
    • •
  • 3 093 tis. Kč
    • •
  • 3 003 tis. Kč
    • •
  • GA ČR
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