Far-field effects of Late Miocene subduction in the Eastern Carpathians: E-W compression and inversion of structures in the Alpine-Carpathian-Pannonian region
Article Abstract:
Late Miocene paleostress data from the Alpine-Carpathian-Pannonian region present evidence of a homogeneous E-W compressive stress field in the brittle upper crust. Compression occurred between 9 Ma and 5.3 Ma and was coeval with late-stage west-directed subduction of the European plate below the Eastern Carpathians. During Late Miocene soft collision, E-W compressive stress was transmitted from the eastern Carpathian plate boundary to the Pannonian Basin and into the Eastern Alps. The basic tectonic effects of the stress field on the area are discussed.
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1997
User Contributions:
Comment about this article or add new information about this topic:
Models for relative motion of crustal blocks within the Carpathian region, based on restorations of the outer Carpathian thrust sheets
Article Abstract:
A rigid block model and back arc extension model of the relative motion of the crustal blocks within the Carpathian region has been developed. The models perform palinspastic restorations of the outer Carpathians thrust sheets. Thrust transport directions changing with time and divergent transport directions are combined to minimize the required arc-parallel extension. Data from the thrust sheet restorations are used to reconstruct block motions for the Pannonian basin, Adriatic block and the Balkans.
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1996
User Contributions:
Comment about this article or add new information about this topic:
Evolution of the transport direction of the Carpathian belt during its collision with the east European Platform
Article Abstract:
A structural analysis of the transition area between the south Carpathians and the east Carpathians is presented, characterizing the strike-slip fault pattern, and revealing its links with the thrust deformation close by. The study of the Pliocene-quaternary deformation aims to provide information on the evolution of the Carpathian belt transport during the Neogene.
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1999
User Contributions:
Comment about this article or add new information about this topic:
- Abstracts: Rheology predictions across the western Carpathians, Bohemian massif, and the Pannonian basin: Implications for tectonic scenarios
- Abstracts: Structural outline of a Tertiary basement-cored uplift/inversion structure in western Spitsbergen, Svalbard: kinematics and controlling factors
- Abstracts: Tectonic burial, thrust emplacement, and extensional exhumation of the Cabot nappe in the Appalachian hinterland of Cape Breton Island, Canada
- Abstracts: The low-pressure stability of phase A, Mg7Si2O8(OH)6. Thermal expansivities and compressibilities of hydrous phases in the system MgO-SiO2-H2O: talc, phase A and 10-angstrom phase
- Abstracts: Chlorine, titanium and barium-rich biotites: factors controlling biotite composition and the implications for garnet-biotite geothermometry