Μorphometric Analysis for the Assessment of Relative Tectonic Activity in Evia Island, Greece [PDF]
Geosciences, 2020 The aim of this study is to evaluate the relative tectonic activity in the north part of the Evia Island, located in Central Greece, and to investigate the contribution of neotectonic processes in the development of the fluvial landscape.
Kanella Valkanou +5 more
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Relative tectonic activity classification in the Kermanshah area, western Iran [PDF]
Solid Earth, 2014 Due to the closing of the subduction zone and the collision of the Arabian and Eurasian plates, the High Zagros region has always been affected by a wide range of tectonic variations.
M. Arian, Z. Aram
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Analysis of Relative study of active tectonics using tectonic morphotectonic indices in the southeastern basins of Bazman volcanic zone [PDF]
مخاطرات محیط طبیعی, 2021 Bazman volcano, in the South East of Iran, northwest of the city of Iranshahr and is located in the north of the city Bazman. The aim of this study was active tectonic basinemanating from the Bazman volcano (with a focus over the city Bazman) and its ...
Shahram Habibi Mood +4 more
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Relative tectonic activity assessment of the Northern Sumatran Fault using geomorphic indices
Frontiers in Earth Science, 2022 Geomorphic indices have widely been applied to assess relative tectonic activity. The relative tectonic activity is mainly associated with relative uplift and long-term tectonic deformation.
Aldo Febriansyah Putra +2 more
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Quantitative analysis of relative tectonic activity in the Acıgöl fault, SW Turkey [PDF]
Arabian Journal of Geosciences, 2018 This study was conducted in order to determine the relative tectonic activity of the Acigol Fault using geomorphic indices. The Acigol Fault is approximately 50 km long and was separated into four segments. For this purpose, the following geomorphic indices have been used: (1) mountain-front sinuosity (Smf), (2) valley floor width-to-valley height ...
Savas Topal
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Towards quantifying the relative tectonic activity in the Trans-Yamuna segment of NW Himalaya [PDF]
Geocarto International, 2023 Owing to the increased availability of high-resolution satellite data and the rapid development of Geographic Information System (GIS) technology, the mapping of active faults and quantification of tectonic activity in inaccessible regions has ...
Swakangkha Ghosh +4 more
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Geomorphic signature of active tectonics in Simav Graben: An evaluation of indicator relative tectonic activity of Simav Fault and its seismotectonic implications for Western Anatolia [PDF]
Journal of Earth System Science, 2023 The main objective of this study is to analyze geomorphic landforms and quantitatively measure various geomorphic parameters to investigate the relative tectonic activity, vertical slip rate, and uplift rate of the Simav Fault. The Simav Fault, which is similar to 25 km long and morphologically composed of five mountain fronts forms the NW section of ...
Mustafa Softa +2 more
exaly +6 more sources
Application of Geomorphic Signatures in Relative Tectonic Activity Assessment of a Red Sea Coastal Basin between Al Farrah and Heelan, Saudi Arabia [PDF]
Applied SciencesThis work used an analysis of the geomorphic indices to effectively assess the relative tectonic activity of a Red Sea coastal region in Saudi Arabia between Al Farrah and Heelan.
Bashar Bashir, Abdullah Alsalman
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Quantitative assessment of relative tectonic activity in the eastern Bandung Basin, Indonesia
Geology, Ecology, and LandscapesThe Eastern Bandung Basin is composed of predominantly Quaternary volcanic rocks and is influenced by tectonic activity. This research aims to determine and evaluate the morphotectonic characteristics and its implication to the potential geological ...
Pradnya Paramarta Raditya Rendra +4 more
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Geologica Acta, 2019 The left-lateral strike-slip Adıyaman fault is located in eastern Turkey within the plate boundary deformation zone between Arabia and Anatolia. The Adıyaman fault is a major splay from the East Anatolian Fault (EAF), one of the most important tectonic ...
A. Khalifa +3 more
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