Results 11 to 20 of about 785 (95)
Geochemistry, Geophysics, Geosystems, 2012 International audienceThe Ganos fault is the westernmost segment of the North Anatolian Fault that experienced the Mw = 7.4 earthquake of 9 August 1912.
Aksoy, M. Ersen +5 more
core +6 more sources
Buried Aseismic Slip and Off-Fault Deformation on the Southernmost San Andreas Fault Triggered by the 2010 El Mayor Cucapah Earthquake Revealed by UAVSAR. [PDF]
Earth Space Sci, 2021 Abstract We use UAVSAR interferograms to characterize fault slip, triggered by the Mw 7.2 El Mayor‐Cucapah earthquake on the 1 San Andreas Fault in the Coachella Valley providing comprehensive maps of short‐term geodetic surface deformation that complement in situ measurements. Creepmeters and geological mapping of fault offsets on Durmid Hill recorded
Parker J +7 more
europepmc +2 more sources
Tectonics, Volume 42, Issue 12, December 2023., 2023 Abstract Subduction forearcs are subject to seismic hazard from upper plate faults that are often invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore requires integration of geomorphic, geologic, and paleoseismic data. We demonstrate the utility of a combined approach in a densely populated region of Vancouver
Nicolas Harrichhausen +10 more
wiley +1 more source
Tectonics, Volume 42, Issue 9, September 2023., 2023 Abstract The NE‐dipping Anghiari normal fault, bounding to the west the Sansepolcro basin in the Upper Tiber Valley (northern Apennines), is thought to be a synthetic splay of the Altotiberina low‐angle normal fault (LANF), an active ENE‐dipping extensional detachment whose seismogenic behavior is debated.
A. Testa +11 more
wiley +1 more source
Sedimentary Records of Liquefaction: Implications From Field Studies
Journal of Geophysical Research: Earth Surface, Volume 128, Issue 8, August 2023., 2023 Abstract The susceptibility of grains in sediment to the liquefaction process causes the development of deformation structures. Some sediments undergo liquefaction, others do not. There is a group of sediments especially prone to liquefaction, which was proven during laboratory experiments.
Szymon Świątek +3 more
wiley +1 more source
Tectonics, Volume 42, Issue 6, June 2023., 2023 Abstract The Trans‐Mexican Volcanic Belt is an active continental volcanic arc related to subduction along the Middle America trench. It is characterized by intra‐arc extension resulting into several major arc‐parallel active fault systems and tectonic basins.
Rodrigo León‐Loya +10 more
wiley +1 more source
On the Inference of Tsunami Uncertainties From Landslide Run‐Out Observations
Journal of Geophysical Research: Oceans, Volume 127, Issue 4, April 2022., 2022 Abstract Probabilistic tsunami hazard analysis (PTHA) due to submarine landslides is much less developed than PTHA for earthquake sources. This is partly because of less constrained data available for quantifying source probability, and partly because of the lack of knowledge related to the tsunami generation process due to landslide dynamics.
T. Zengaffinen‐Morris +2 more
wiley +1 more source
Segmentation and Holocene Behavior of the Middle Strand of the North Anatolian Fault (NW Turkey)
Tectonics, Volume 40, Issue 11, November 2021., 2021 Abstract The North Anatolian Fault (NAF) in the Marmara region is composed of three parallel strands all separated by ∼50 km. The activity of the middle strand, which borders the southern edge of the Marmara Sea, is much debated because of its present‐day very low seismicity. This contrasts with historical, archeological and paleoseismological evidence,
Y. Benjelloun +4 more
wiley +1 more source
An integrated geodetic and InSAR technique for the monitoring and detection of active faulting in southwestern Sicily [PDF]
, 2020 We present the results of the analysis of GNSS (Global Navigation Satellite System) and InSAR (Interferometric synthetic-aperture radar) data collected in the frame of a project financed by the “Struttura Terremoti” of INGV (Istituto Nazionale di ...
Barreca Giovanni +7 more
core +1 more source