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391 (0,089s) •

Project

The role of inherited continental margin architecture on early Variscan convergence (GA17-22207S)

It is well known that the inherited architecture of extended continental margins controls the collisional processes and deformation structure of ensuing orogens. However, the classical hyperextended margins of the Atlantic...

DB - Geologie a mineralogie

  • 2017 - 2021
    • •
  • 6 637 tis. Kč
    • •
  • 6 250 tis. Kč
    • •
  • GA ČR
Project

Volcanism related to the breakdown of the passive continental margin, an example from the southern part of the Vrbno Group, Silesicum (GA205/01/0331)

Petrologie and geochemical character of volcanic rocks - especially basic ones - are sensitive indicators of their geotectonic and palaeogeographic settings. Volcanic rocks suitable for such a study occur in the Devonian sedimentary basins at the NE ...

DB - Geologie a mineralogie

  • 2001 - 2003
    • •
  • 2 058 tis. Kč
    • •
  • 1 384 tis. Kč
    • •
  • GA ČR
Project

Origin of the relaminant in the Bohemian Massif during the Variscan orogeny (GA23-08249S)

or magma-rich passive margin, and continental or oceanic magmatic arc. For decisions identified as magmatic arcs and possibly as magma-rich passive margin.......

Geology

  • 2023 - 2025
    • •
  • 6 579 tis. Kč
    • •
  • 6 579 tis. Kč
    • •
  • GA ČR
Project

Seismicity pattern as indicator of source regions of volcanism at convergent plate margins (IAA3012303)

margins. Datasource: Relocated earthquake hypocentre parameters of the International-Benioff zonefrom those located in the continental wedge below active volcanoes; time plate margins, and of the position of source region ...

DC - Seismologie, vulkanologie a struktura Země

  • 2003 - 2006
    • •
  • 2 308 tis. Kč
    • •
  • 1 241 tis. Kč
    • •
  • AV ČR
Project

Changes of rheology of the lower and middle crust during orogenic processes - example of the north-eastern margin of the Bohemian Massif (GA205/99/1195)

Marginal parts of orogens on the contact between orogenic root domain with surrouding continental crust are characterized by specific thermomechanical evolution, which is dependent on thermal age of the crust, lithological stratific...

DB - Geologie a mineralogie

  • 1999 - 2001
    • •
  • 698 tis. Kč
    • •
  • 648 tis. Kč
    • •
  • GA ČR
Project

Black shale formations as geochemical markers of paleoenvironmental changes and tectonic setting along active continental margins (GA17-15700S)

their potential as stratigraphic markers in accretionary systems at convergent plate margins...

DD - Geochemie

  • 2017 - 2019
    • •
  • 10 688 tis. Kč
    • •
  • 9 689 tis. Kč
    • •
  • GA ČR
Project

Principal mechanisms of peripheral continental growth during supercontinent cycle (GX19-27682X)

The growth of eastern Pangea involves three contrasting orogenic cycles: 1) Baikalian cycle (570-540 Ma) consists of accretion of peri-Rodinian continental, Mirovoi and Panthalassan oceanic fragments to the Siberian margin followed ...

Geology

  • 2019 - 2024
    • •
  • 43 501 tis. Kč
    • •
  • 43 501 tis. Kč
    • •
  • GA ČR
Project

Dynamics of Precambrian accretionary wedges and mélanges (GP14-10589P)

with a number of broad implications for studies on subduction zone and active continental margin dynamics....

DB - Geologie a mineralogie

  • 2014 - 2018
    • •
  • 3 377 tis. Kč
    • •
  • 3 377 tis. Kč
    • •
  • GA ČR
Project

Seismotectonics and deep structure of Middle American convergent plate margin (GA205/03/1203)

continental wedge....

DC - Seismologie, vulkanologie a struktura Země

  • 2003 - 2005
    • •
  • 1 995 tis. Kč
    • •
  • 960 tis. Kč
    • •
  • GA ČR
Project

International Continental Scientific Drilling Program - ICDP (LA 150)

Investigation of structure and dynamics of the upper layers of the continental Earth crust by means of deep drilling, , ,...

DC - Seismologie, vulkanologie a struktura Země

  • 2002 - 2006
    • •
  • 4 758 tis. Kč
    • •
  • 4 118 tis. Kč
    • •
  • MŠMT
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