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- > Neotectonics and active faulting (supprimer)
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Par Collection Par Auteur- STEWART, I., (Editeur scientifique) (3)
- GAKI-PAPANASTASSIOU, K. (1)
- MAROUKIAN, H. (1)
- PIJET, E. (1)
- KRZYSZKOWSKI, D. (1)
- MCCALPIN, J.P. (1)
- PAPANASTASSIOU, D. (1)
- 1993 (3)
- Archaeology ; Earthquake ; Fault ; Greece ; Quaternary ; Structural geomorphology ; Tectonics (1)
- Archéologie ; Faille ; Grèce ; Géomorphologie structurale ; Quaternaire ; Séisme ; Tectonique (1)
- Drainage network ; Fault ; Neotectonics ; Pleistocene ; Poland ; Sudety ; Vertical movement (1)
- Earthquake ; Fault ; Model ; Neotectonics ; Palaeogeography ; Quaternary ; Tectonics ; United States ; Western United States (1)
- Etats-Unis ; Etats-Unis de l'Ouest ; Faille ; Modèle ; Néotectonique ; Paléogéographie ; Quaternaire ; Séisme ; Tectonique (1)
- Faille ; Mouvement vertical ; Néotectonique ; Pléistocène ; Pologne ; Réseau de drainage ; Sudety (1)
- Neotectonics and active faulting (3)
- Morphological effects of Pleistocene fault activity in the Sowie Mts., southwestern Poland (1)
- Morphotectonic and archaeological observations in the eastern Argive Plain (eastern Peloponnese, Greece) and their palaeoseismological implications (1)
- Neotectonics of the northeastern Basin and Range margin, western USA (1)
- Neotectonics of the northeastern Basin and Range margin, western USA
- Eleven backhoe trenches were excavated across six Quaternary fault scarps on the northeastern margin of the Basin and Range extensional tectonic province. Fifteen palaeoseismic events can be recognized, bracketed by radiocarbon or thermoluminescence
- This paper discusses the morphological and geological evidence for Pleistocene neotectonic faulting and uplift in the northeastern part of the Sowie Mountains where the Sudetic Marginal Fault has its maximum deplacement and uplift rates. Although
- , river channels, alluvial cones and fans and slope failures with archaeological evidence of seismic events at the Acropolis along the eastern margin of the Argive Plain in order to obtain an improved understanding of the paleoseismicity of this region.