Results 41 to 50 of about 3,134 (203)

Morphotectonics of Myzotska Upland

Visnyk of the Lviv University. Series Geography, 2014
The aim of this work is the interpretation results of morphotectonic analysis of Myzotska Upland for investigation its neotectonic history and identifying regional morphotectonic differences. We used planed surface reconstruction method and stream gradient index (SL index).
Taras Novak, Andriy Bermes
openaire   +2 more sources

The active Nea Anchialos Fault System (Central Greece): comparison of geological, morphotectonic, archaeological and seismological data

Annals of Geophysics, 1996
The Nea Anchialos Fault System has been studied integrating geological, morphological, structural, archaeological and seismic data. This fault system forms the northern boundary of the Almyros Basin which is one of the Neogene-Quaternary tectonic basins ...
R. Caputo
doaj   +1 more source

Rates of erosion and landscape change along the Blue Ridge escarpment, southern Appalachian Mountains, estimated from in situ cosmogenic 10Be [PDF]

, 2016
The Blue Ridge escarpment, located within the southern Appalachian Mountains of Virginia and North Carolina, forms a distinct, steep boundary between the lower-elevation Piedmont and higher-elevation Blue Ridge physiographic provinces.
Bierman, Paul R., Finkel, Robert C., Freeman, Stewart P.H.T., Linari, Colleen L., Pavich, Milan J., Portenga, Eric W.   +5 more
core   +2 more sources

Morphotectonic affilation of the Lilyak Plateau

Acta Scientifica Naturalis, 2022
Abstract The morphostructural features of the Lilyak Plateau and it’s spatial and morphotectonic relationships with the adjacent parts of the Eastern Pre-Balkan Mountains are examined in the light of modern mobilist ideas. The Lilyak Plateau landform is part of the South Moesian morphostructural zone.
Svetla Stankova, Tzanko Tzankov
openaire   +1 more source

Sedimentation record in the Konkan-Kerala Basin: implications for the evolution of the Western Ghats and the Western Indian passive margin [PDF]

, 2007
The Konkan and Kerala Basins constitute a major depocentre for sediment from the onshore hinterland of Western India and as such provide a valuable record of the timing and magnitude of Cenozoic denudation along the continental margin.
Allen P.A., Auden J.B., Balakrishnan T.S., Cox K.G., Drury S.A., Ghosh B.N., Gilchrist A.R., Gunnell Y., Gunnell Y., Gunnell Y., Gunnell Y., Hetenyi M., Joseph S., Kalaswad S., Kearey P., King L.C., King L.C., Krishnan M.S., Mathur R.B., McHargue T.R., Naini B.R., Nair K.M., Naqvi S.M., Ollier C.D., Ollier C.D., Pascoe E.H., Persano C., Radhakrishna B.P., Radhakrishna B.P., Raju D.S.N., Rao P.R., Rao S.V., Rao V.P., Schlich R., Singh N.K., Stephen J., Stuwe K., Summerfield M.A., Turcotte D.L., Vaidyanadhan R., Watts A.B., Widdowson M., Widdowson M., Widdowson M.   +43 more
core   +1 more source

Neogene drainage evolution of SW Anatolia (Türkiye): Integration of morphotectonics, drainage and denudation analyses

Earth Surface Processes and Landforms
This study integrates denudation analysis with morphotectonic characteristics, facies associations and drainage analysis to investigate the landscape evolution of SW Anatolia.
P. V. van Heiningen, Nuretdin Kaymakçı
semanticscholar   +1 more source

New ideas about the Balkan peninsula East Part morphotectonics

Acta Scientifica Naturalis, 2020
The article introduces the results of the author’s new investigations about the origin, Quaternary morphotectonic evolution and the modern morphostructure of the Bulgarian Continental Microplate in the eastern part of Balkan Peninsula.
T. Tzankov, S. Stankova
semanticscholar   +1 more source

MORPHOSTRUCTURE OF THE KODAR-UDOKAN SECTION OF THE BAIKAL RIFT ZONE

Geography, Environment, Sustainability, 2014
The morphostructure of the region is a natural result of active geodynamics in the eastern Stanovoe Upland. Extreme seismic conditions become apparent in rare devastating earthquakes (up to 10-11 in the Mercally scale), as well as in frequent slight ones.
Andrey A. Lukashov, Stepan V. Maznev
doaj   +1 more source

Structural Controls on Splay Fault Rupture Dynamics During Cascadia Megathrust Earthquakes

AGU Advances, Volume 6, Issue 6, December 2025.
Abstract Great subduction earthquakes (Mw ≥ 8.0) can generate devastating tsunamis by rapidly displacing the seafloor and overlying water column. These potentially tsunamigenic seafloor offsets result from coseismic fault slip and deformation beneath or within the accretionary wedge. The mechanics of these shallow rupture phenomena and their dependence
J. Biemiller, A.‐A. Gabriel, L. Staisch, T. Ulrich, A. Dunham, E. Wirth, J. Watt, M. C. Lucas, A. Ledeczi   +8 more
wiley   +1 more source

Morphotectonic evolution of the Jebel Bou Naceur in the South Middle Atlas Fault Zone (Morocco) [PDF]

, 2007
International audienceIn eastern Morocco, fault-related folds develop above the South Middle Atlas fault that separates the J. Bou Naceur 'pop-up' structure and the Missour Basin, filled with alluvial sediments.
Amrhar, M., Carozza, Jean-Michel, Charroud, M., Delcaillau, Bernard, Dugué, Olivier, Laville, E.   +5 more
core   +5 more sources