Results 1 to 10 of about 8,222 (215)

Tracing woody-organic tsunami deposits of the 2011 Tohoku-oki event in Misawa (Japan) [PDF]

open access: yesScientific Reports, 2021
With a minimum of three reported waves, the 2011 Tohoku-oki tsunami’s destructive force caused massive damage along the northern Japanese Aomori coast. At Misawa the coastal control area was inundated up to 550 m inland and sandy sediment remnants can be
Piero Bellanova   +4 more
doaj   +2 more sources

The Active Faults of Eurasia Database (AFEAD): the ontology and design behind the continental-scale dataset [PDF]

open access: yesEarth System Science Data, 2022
Active faults are those faults on which movement is possible in the future. This draws particular attention to active faults in geodynamic studies and seismic hazard assessment.
E. Zelenin   +5 more
doaj   +1 more source

Jovan Cvijic: Forefather of neotectonics [PDF]

open access: yesZbornik Radova: Geografski institut "Jovan Cvijić", 2003
Neotectonic activity as crucial factor of geomorphological evolution represents nowadays widely reckognized fact. It is generaly believed and accepted that the study of neotectonics began during first half of the 20th century by Russian scientists in the
Marković Miroslav
doaj   +1 more source

Motion maps derived from optical satellite images: the case study of the East Anatolian Fault (Türkiye) [PDF]

open access: yesBrazilian Journal of Geology, 2023
On February 6, 2023, two earthquakes shook the southern and central Türkiye causing significant loss of human life and devastating many cities. These are related to the active East Anatolian Fault (EAF). In this study, the digital image correlation (DIC)
Marcos Eduardo Hartwig   +2 more
doaj   +1 more source

Landslide susceptibility mapping by using a geographic information system (GIS) along the China–Pakistan Economic Corridor (Karakoram Highway), Pakistan [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2019
The Karakoram Highway (KKH) is an important route, which connects northern Pakistan with Western China. Presence of steep slopes, active faults and seismic zones, sheared rock mass, and torrential rainfall make the study area a unique geohazards ...
S. Ali   +4 more
doaj   +1 more source

Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain

open access: yesAnnals of Geophysics, 2014
The Padul-Nigüelas Fault Zone (PNFZ) is situated at the south-western mountain front of the Sierra Nevada (southern Spain) in the Internal Zone of the Betic Cordilleras and belongs to a NW-SE trending system of normal faults dipping SW.
Jochen Hürtgen   +3 more
doaj   +1 more source

3-D visualisation of palaeoseismic trench stratigraphy and trench logging using terrestrial remote sensing and GPR – a multiparametric interpretation [PDF]

open access: yesSolid Earth, 2016
Two normal faults on the island of Crete and mainland Greece were studied to test an innovative workflow with the goal of obtaining a more objective palaeoseismic trench log, and a 3-D view of the sedimentary architecture within the trench walls ...
S. Schneiderwind   +4 more
doaj   +1 more source

Tectonic structure of Kerch-Taman fold zone of Azov-Kuban trough

open access: yesВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, 2021
The nrotectonic structure of the Kerch-Taman folded zone, the southern deformed part of the Azov-Kuban piedmont trough, has a number of structural features and a history of deformation development.
Гайдаленок О.В.   +2 more
doaj   +1 more source

Neotectonics of the Sumatran fault, Indonesia [PDF]

open access: yes, 2000
The 1900-km-long, trench-parallel Sumatran fault accommodates a significant amount of the right-lateral component of oblique convergence between the Eurasian and Indian/Australian plates from 10°N to 7°S.
Natawidjaja, Danny, Sieh, Kerry
core   +2 more sources

Evidence of Quaternary tectonics along Río Grande valley, southern Malargüe fold and thrust belt, Mendoza, Argentina [PDF]

open access: yes, 2019
The Malargüe fold and thrust belt is developed in the Argentinian Andes between 34° and 37° S, through the tectonic inversion of Upper Triassic and Lower Jurassic depocenters of the Neuquén Basin, with an uplift history since the Cretaceous.
Colavitto, Bruno   +4 more
core   +1 more source

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