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Analytical Solution for the Stress Field in Surrounding Rock of a Near-Fault Tunnel Considering Tectonic Stress Boundary Conditions
In the existing analytical solutions for tunnels, the tectonic stress boundary conditions caused by faults are often overlooked. This study presents...
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Assessment of the relative tectonic activity of the Longxian–Baoji Fault Zone in the northeastern Tibetan Plateau based on geomorphic indices
Since the Late Cenozoic, tectonic deformation has been intense in the Longxian–Baoji Fault Zone (LBFZ), which is at the intersection of the southwest...
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Recent Reactivation of Variscan Tectonic Zones: A Case of Rodl-Kaplice-Blanice Fault System (Bohemian Massif, Austria/Czech Republic)
The Rodl-Kaplice-Blanice fault system (RKB) of Variscan shear origin, repeatedly active since the Late Paleozoic to the Recent, is expressed by a...
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Numerical simulation of tectonic stress and strain rate fields in the northeastern margin of the Tibetan Plateau in association with major fault zones
A series of large strike-slip and thrust faults have developed in the northeastern margin of the Tibetan Plateau since the Late Cenozoic, with strong...
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Geomorphic signature of active tectonics in Simav Graben: An evaluation of indicator relative tectonic activity of Simav Fault and its seismotectonic implications for Western Anatolia
The main objective of this study is to analyze geomorphic landforms and quantitatively measure various geomorphic parameters to investigate the...
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The Causes of Tectonic and Seismic Activity of the Liskin Fault Zone (the Southeastern Voronezh Uplift, the East European Platform)
AbstractThe Liskin fault zone located in the southeastern part of the East European Platform at the boundary between two large neotectonic...
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Fault Striae Analysis and Paleostress Reconstruction of the Northern Tectonic Province (Egyptian Nubian Shield): Insights into the Brittle Deformation History of the Northern East African Orogen
AbstractThe Egyptian Nubian Shield (ENS), the northwestern continuation of the East African Orogen (EAO), comprises a variety of three lithologically...
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Sedimentary and tectonic evolution of the Banquan pull-apart basin and implications for late Cenozoic dextral strike-slip movement of the Tanlu Fault Zone
The Banquan Basin is a pull-apart basin with the largest scale and the most prominent structure due to dextral slip of the Tanlu Fault Zone (TLFZ) in...
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Cenozoic tectonic evolution of regional fault systems in the SE Tibetan Plateau
The SE Tibetan Plateau, tectonically situated in the eastern India-Eurasia oblique convergence zone, has experienced multiple stages of deformation...
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Tectonic Regime as a Control Factor for Crustal Fault Zone (CFZ) Geothermal Reservoir in an Amagmatic System: A 3D Dynamic Numerical Modeling Approach
Crustal fault zones provide interesting geological targets for high-temperature geothermal energy source in naturally deep-fractured basement areas....
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Tectonic framework and fault structures in the Fagradalsfjall segment of the Reykjanes Peninsula Oblique Rift, Iceland
The two volcanic eruptions of 2021 and 2022 at Fagradalsfjall in SW Iceland occurred within the Reykjanes Peninsula Oblique Rift, a segment of the...
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Reconstruction of the deformation history of an active fault: implications from the Atera Fault, Central Japan
Atera Fault clay gouges were collected for age dating near Kawaue, Nakatsugawa City, Central Japan, and the results integrated within its complex...
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Seismicity characteristics of secondary faults in the Zhangjiakou-Bohai tectonic zone
We have systematically sorted out the seismic events of each secondary fault and its surroundings in the Zhangjiakou-Bohai tectonic belt and jointly...
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Evaluation of the Relative Tectonic Activity from the Faults in the Gengma-Lancang-Menghai Seismic Belt (Southwestern China)
The Gengma-Lancang-Menghai seismic belt, the southernmost part of the North-South seismic belt, is controlled by four active faults: the Nantinghe...
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Volcanism and Tectonic Setting
Since publication of Cas and Wright (1987), the relationship between volcanism and tectonic setting has expanded into an enormous and... -
Current active fault distribution and slip rate along the middle section of the Jiali-Chayu fault from Sentinel-1 InSAR observations (2017–2022)
The Jiali-Chayu fault, situated on the eastern side of the eastern Himalayan syntaxis, is the southeastern margin of the large strike-slip fault zone...
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Observing tectonic-geomorphological changes along the Dawki Fault and adjoining areas of Sylhet, Bangladesh from 1980 to 2020 using remote sensing and GIS techniques
AbstractIn this paper, we observed the tectono-geomorphological changes along the Dawki Fault and adjoining areas of Sylhet, Bangladesh using...
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FRS (Fault Rating System): a quantitative classification of active faults for hazard evaluations
AbstractThe correct estimation of seismic hazards is a touchstone of seismic risk assessments. However, there is no quantitative or standard...
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Active tectonic deformation and its seismic–geological significance of boundary faults of the Daxing Uplift and Langgu–Dachang Depression, Bei**g Plain, China
Boundary faults of the Daxing Uplift and Langgu–Dachang Depression are located in the southeastern region of the Bei**g Plain and directly control...
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Tectonic pattern and relative age of Ba-rich veins in front of a poly-deformed Precambrian inlier (Saghro, Morocco)
The present study reports the first structural analysis of tectonic-controlled ore deposits in the Paleozoic southern flank of the Saghro massif...