Results 51 to 60 of about 105 (95)
Is the Suez Rift in Its Post‐Rift Phase?
Abstract Failed rifts are widely assumed to enter post‐rift tectonic quiescence after termination of intracontinental rifting, but a comprehensive understanding of their regional morphotectonics is lacking. Our quantitative, rift‐scale geomorphic analyses in the Suez Rift, an archetypal failed rift in Egypt, reveals widespread rifting after presumed ...
David Fernández‐Blanco +2 more
wiley +1 more source
Abstract In a subduction zone, variability in the buoyancy and structure of the downgoing plate impacts deformation patterns in the overriding plate. Thick and buoyant lithosphere or smaller‐scale indentors entering the trench can lead to significant relief development and exhumation. To investigate such processes, we target the Cenozoic reorganization
E. M. Conrad, C. Faccenna, D. F. Stockli
wiley +1 more source
Controls on Water‐Magma Interactions at Hydraulically‐Charged Volcanic Islands
Abstract The interaction of rising magma with groundwater can produce phreatomagmatic explosions, which, given their enhanced explosivity and unpredictability, increase the hazard potential of volcanic eruptions. To investigate the link between groundwater occurrence and phreatomagmatism, we compare the volcanic record of Flores Island (Azores) with ...
M. Andrade +7 more
wiley +1 more source
Abstract The spatial distribution of seismicity in active fault zones depends primarily on the geometry of the fault networks. However, recent advances suggest that seismic activity may also be controlled by the rheology of the geological units surrounding fault zones. In the present work, we use seismological and geological analyses to investigate the
Maxime Godano +9 more
wiley +1 more source
This study aims to find possible active faults by analysing the morphotectonic features of the Cikandang Watershed in West Java, Indonesia. Morphometric indices including drainage density (Dd), lineament density (Ld), and bifurcation ratio (Rb) were ...
Ghina H. Fahira +2 more
doaj +1 more source
Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
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
Abstract The Hellenic forearc is one of the least understood forearc systems globally due to limited availability of high‐resolution imagery of its deep structure, especially landward of the Mediterranean Ridge. Here, we combine widely spaced high‐resolution multichannel seismic‐reflection profiles with seafloor morpho‐bathymetric analysis and ...
Vasiliki Mouslopoulou +7 more
wiley +1 more source
Morphotectonics of the Pescara River basin (Central Italy)
This work presents a morphotectonic map of the Pescara River basin (1:40,000 scale), located in the piedmont-hilly area of the central-eastern Apennines (Abruzzo Region, Italy), and stretching from the eastern slope of the chain (Maiella Massif, Morrone ...
Tullio Urbano +2 more
doaj +1 more source
The research focuses on revealing the main morphotectonic expressions of relief, as a contribution to the study of moderate seismicity of territory. Morphostructural analysis combined with results of analysis of structures, to mesoscopic scale, provide ...
Alexis Ordaz Hernández +4 more
doaj +1 more source
Anthropogenic interventions on land neutrality in a critically vulnerable estuarine island ecosystem: a case of Munro Island (India). [PDF]
Rafeeque MK +5 more
europepmc +1 more source

