Results 61 to 70 of about 11,203 (214)
The 2005 - 2007 Bala (Ankara, central Turkey) earthquakes : a case study for strike-slip fault terminations [PDF]
, 2014 An intense seismic activity has been observed after the Bala (Ankara, NW central Turkey) earthquakes (30 July 2005: Mw=5.3, 20 December 2007: Mw=5.4, and 26 December 2007: Mw=5.3), continuing up to the present.
Ecevitoglu, B. +5 more
core +3 more sources
FMLD: A Vertical Federated Learning Framework for Privacy‐Preserving Multimodal Landslide Detection
Journal of Geophysical Research: Machine Learning and Computation, Volume 3, Issue 1, February 2026.Abstract Landslides are among the most severe global geohazards posing a significant threat to human life and infrastructure. To support landslide detection and prediction, various geohazard monitoring approaches have been developed, such as optical remote sensing imagery, light detection and ranging, and ground‐based sensors, generating vast volumes ...
Xiaochuan Tang +11 more
wiley +1 more source
Neotectonics of the San Andreas fault system: Basin and range province juncture [PDF]
Several new details regarding the surficial patterns of neotectonic activity of the Eastern Transverse Ranges and vicinity were discovered. Additionally a number of data display and analysis techniques were developed.
Crowell, J. C., Estes, J. E.
core +5 more sources
Neotectonics of the Manych Trough
Doklady Earth Sciences, 2011 The general (regional) and local neotectonic features of the Manych Trough have been discussed. It has been shown that the trough’s bottom was generally immersed at a slow but stable rate of 0.1 mm/year with an amplitude of 40–50 m. Additionally, migration of portions of the maximal and minimal immersion has been identified.
A. A. Svitoch, R. R. Makshaev
openaire +1 more source
Geochemistry, Geophysics, Geosystems, Volume 27, Issue 1, January 2026.Abstract This study presents a soil gas geochemical survey in the Kırcaoğlu and Reyhanlı regions of Hatay Province, southeastern Türkiye, following the 2023 Kahramanmaraş earthquake doublet. The aim was to identify concealed faults and assess seismic hazard through analysis of soil CO2 flux, CO2 and 222Rn concentrations, and carbon and helium isotopic ...
G. Yüce +16 more
wiley +1 more source
Actividad de la falla la salina a partir de instrumentación sismológica
Earth Sciences Research Journal, 2003 <p class="MsoNormal" style="line-height: normal; margin: 0cm 0cm 0pt; mso-layout-grid-align: none;"><span style="font-family: ";Arial";,";sans-serif";; font-size: 12pt; mso-ansi-language: EN-US;" lang="EN-US">The "La Salina" Fault, located in
Gómez Ernesto +1 more
doaj
Neotectonics of the Sumatran fault, Indonesia [PDF]
, 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
Crustal Structure Across the Okavango Rift, Botswana: The SEISORZ Wide‐Angle Seismic Experiment
Journal of Geophysical Research: Solid Earth, Volume 131, Issue 1, January 2026.Abstract The Okavango Rift Zone (ORZ) is an incipient continental rift in Botswana at the terminus of the Southwestern Branch of the East African Rift System. The lack of syn‐rift magmatism and tectonic processes overprinting pre‐rift structures provide an opportunity to investigate incipient‐stage rift processes and the role of pre‐existing structures
J. Pablo Canales +7 more
wiley +1 more source
Neotectonic study of Northwestern Greece
Journal of Maps, 2018 In this paper, a neotectonic map with active faults, at a scale of 1:500,000, of the northwestern Greece is presented and discussed. The elaboration of the Neotectonic Map chiefly aimed at the identification, mapping and assessment of the faults in the ...
Dimitrios Ntokos
doaj +1 more source
Tectonic Structure of the Island of Hvar (Southern Croatia)
Geologia Croatica, 2010 Structural deformation of the island of Hvar allows three tangentialtectonic phases to be determined: the Laramian (F I), the Pyrenean,( F II) and the Neotectonic phase (F III ).
Stanko Marinčić
doaj +1 more source