Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian. [PDF]
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 ...
Owen, Lewis +6 more
openaire +4 more sources
GIS-Analysis for Active Tectonics Assessment of Wadi Al-Arish, Egypt
Applied Sciences, 2023 In this paper, we apply an effective method to evaluate relative tectonic activity by applying several morph-tectonic indices that are useful in evaluating topography and tectonics.
Bashar Bashir +3 more
doaj +1 more source
Holocene relative sea-level change along the tectonically active Chilean coast [PDF]
Quaternary Science Reviews, 2020 We present a comprehensive relative sea-level (RSL) database for north, central, and south-central Chile (18.5°S – 43.6°S) using a consistent, systematic, and internationally comparable approach. Despite its latitudinal extent, this coastline has received little rigorous or systematic attention and details of its RSL history remain largely unexplored ...
Garrett, Ed +7 more
openaire +7 more sources
Spatial Analysis of Landslides in Relation to Active Tectonics Based on Morphotectonic Indices in Kheirabad River Basin [PDF]
پژوهشهای آبخیزداری, 2022 Neotectonic activity plays an important role in increasing the occurrence of landslides. The purpose of this study is to investigate the relationship and the extent of landslide occurrence from active tectonics in the Kheirabad River Basin River.
Hamid Babolimoakher
doaj +1 more source
IDENTIFICATION OF GEOMORPHIC SIGNATURES OF NEOTECTONIC ACTIVITY USING DEM IN THE PRECAMBRIAN TERRAIN OF WESTERN GHATS, INDIA [PDF]
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2012 To assess the relative tectonic activity classes, five geomorphic indices such as stream-gradient index (SL), drainage basin asymmetry (Af), hypsometric integral (Hi), valley floor width – valley height ratio (Vf) and drainage basin shape (Bs) of ...
K. S. Jayappa +2 more
doaj +1 more source
TECTONIC GEOMORPHOLOGY OF THE KARANGSAMBUNG AREA, CENTRAL JAVA, INDONESIA
Rudarsko-geološko-naftni Zbornik, 2021 Karangsambung, located in Central Java, Indonesia has complex geological conditions of the tectonic evolution of Java Island due to the subduction process of the India-Australia plate with the Eurasian plate in the Cretaceous-Paleocene.
Edi Hidayat +4 more
doaj +1 more source
Iraqi Geological Journal, 2022 The morphotectonic analysis was done of the Roste valley, within the Imbricated and Suture zone of the Zagros Fold,Thrust Belt. The formations of the Imbricate Zone are of Jurassic and Cretaceous ages and the Suture Zone is covered by Zagros ...
Paiwast Zhazhlayi, Ali Surdashy
doaj +1 more source
Evaluation of Morphotectonic Indices in Qangholichay Basin [PDF]
جغرافیا و آمایش شهری منطقهای, 2017 Neo-tectonic is of dynamic factors which always affects on the watersheds and rivers. Neo-tectonic is said to the new tectonic factors which mainly reflects in the faults. Displacement of faults can trigger the epicenters of the earthquake, the release
Dr.Gholam Hassan Jafari +1 more
doaj +1 more source
Geomorphic response to neotectonic activity in the Jura Mountains and in the southern Upper Rhine Graben [PDF]
, 2008 Present-day tectonic activity at the southern end of the Upper Rhine Graben in central Western Europe is evidenced by significant seismicity, which has been documented over hundreds of years.
Fraefel, Marielle
core +1 more source
Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey) [PDF]
, 2021 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 ...
Çakir, Z. +3 more
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