Results 51 to 60 of about 5,210 (163)
Neotectonic folds in the central-western Peloponnese, Greece
The western Peloponnese, being very close to the Hellenic Trench, is one of the most active areas in Greece. The study area is located at the central western part of Peloponnese and it is developed in a NNW-SSE direction along 45 km, parallel to the ...
Mariolakos, I., Fountoulis, I.
core +1 more source
NEOTECTONICS OF THE SEA OF OKHOTSK
The analysis of the neotectonic structure of the region is usually accompanied by the compilation of neotec‐ tonic maps and schemes. Models of the summit surface serve as the initial material for compiling different‐scale neo‐ tectonic maps and schemes ...
V. P. Semakin +2 more
doaj +1 more source
Active Tectonics of the Eastern and Southern Alps ‐ Crustal Response to Deep Processes? A Review
Abstract Owing to the low N‐S convergence rates between Adria and Europe, crustal deformation rates in the Alps and its forelands are low. Active tectonics are, therefore, difficult to study, especially as non‐tectonic landscape forming processes can erase or modify the tectonic surface imprint. Large‐scale and dense seismological data recently offered
Christoph Grützner +20 more
wiley +1 more source
Neotectonic Movement of the Northern East China Sea Shelf Basin
On the base of comprehensive analysis of some new single-track seismic profiles and logging data, the neotectonic movement characteristics of the northern East China Sea Shelf Basin are researched.
San Zhong Li +2 more
core +1 more source
ABSTRACT Like other perialpine basins and glaciated margins, the Geneva Basin in SW Switzerland is characterised by buried tunnel valleys, which are elongated incisions widely attributed to subglacial meltwater erosion beneath continental ice sheets. However, an inclusive understanding of the geological control on the evolution of the glacial landscape
Ovie Emmanuel Eruteya +2 more
wiley +1 more source
Abstract Uplifted Pleistocene marine terraces in the Illapel area along the forearc of central Chile record spatially and temporally variable uplift rates on glacial‐cycle timescales. However, the underlying mechanisms for this uplift variability and its potential relationship with the megathrust‐earthquake cycle remain poorly understood.
Roland Freisleben +8 more
wiley +1 more source
Tectonic Structure of the Island of Hvar (Southern Croatia)
Structural deformation of the island of Hvar allows three tangentialtectonic phases to be determined: the Laramian (F I), the Pyrenean,( F II) and the Neotectonic phase (F III ).
Stanko Marinčić
doaj +1 more source
Neotectonic Indications from the Western and Southern Deserts of Iraq
The Iraqi Western and Southern deserts are part of the Iraqi Stable Shelf (Inner Platform) that belongs to the Arabian Plate. Therefore, both deserts lack tectonic forms like folds and faults; however, very rarely faults and regional lineaments can be ...
Al-Ansari, Nadhir, +7 more
core +1 more source
Abstract The Cascadia subduction zone can produce M9+ megathrust and M6.5+ intraplate earthquakes, motivating the need for a detailed 3‐D model of seismic properties at scales relevant to regional geology, basins, and infrastructure. To construct the Generation 0 Cascadia Region Earthquake Science Center Community Velocity Model (CRESCENT CVM), we ...
Bin He +12 more
wiley +1 more source
Neotectonic research in applied geomorphological studies
The authors illustrate several methods for geomorphological and morpho-neotectonic analysis focused on different practical ...
CASTALDINI, Doriano +4 more
core +1 more source

