Results 21 to 30 of about 510 (155)
Some thoughts on the morphotectonic development of the Denizli region Basic
Bulletin of the Mineral Research and Exploration, 2022 The Denizli region is located to the east of the Buldan Horst. Although they follow the same trends as the Büyük Menderes and Gediz Grabens, the Denizli region has undergone semi-independent evolution during the Quaternary.
Yücel Yılmaz
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Geogaceta, 2023 The Volubilis piggy-back basin, located at the front of the Rif belt, northern Morocco, is a subsided area, as a continuation of the deformational orogenic ridges, related to the present-day African and Eurasian convergence.
Afaf Amine +4 more
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Geosciences, 2023 This paper presents a morphometric and structural-geomorphological approach to identifying morphotectonic features across an area underlain by lithologies that do not easily record tectonic deformations but are widely affected by seismic activity.
Vania Mancinelli +6 more
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Morphotectonics and resultant features in Kaliani River Basin (Assam) [PDF]
, 2011 The surficial structure and impressions upon the crust due to endogenetic and exogenetic mechanisms are witnessed all around us. These landforms have evolved as a result of plate movements, subsidence, upliftment and various erosional processes.
V.C. Jha, Sucheta Mukherjee
core +1 more source
Geomorphic and archaeological -historical evidence for past ealihquakes in Greece
Annals of Geophysics, 1996 Geomorphic observations focused on landforms of marine and fluvial origin such as notches, beachrocks, stream channel shifts, alluvial terraces and knickpoints, when combined with historical and archaeological information are able to date seismic events ...
H. Maroukian +2 more
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Morphotectonic development of the Marmara Region
Tectonophysics, 2010 Abstract The Marmara Region of northwest Turkey covers the Marmara Sea Basin and the surrounding lands. In the region, morphologically different areas may be distinguished. The Marmara Sea Basin is a structural depression. The land to the north is known as the Thrace-Kocaeli Peneplain, a flatland elevated above a horst. This may be referred to as the
Yılmaz, Yücel +3 more
openaire +2 more sources