Bi-directional extensional control of the Berane Basin formation, northern Montenegro [PDF]
Geološki Anali Balkanskoga PoluostrvaThe Berane Basin is a Miocene, northeast‐southwest oriented intramountain basin of the Dinarides, overlying the pre‐neotectonic basement of the Drina–Ivanjica unit, the East Bosnian–Durmitor unit and the Western Vardar Zone.
Stefanović Katarina +1 more
doaj +1 more source
Origin of superimposed and curved slickenlines in San Miguelito range, Central México [PDF]
, 2013 Interactions between intersecting faults cause local perturbations of the stress field in the vicinity of their intersections. Fault intersections are places of stress accumulation, stress relief and refraction of the stress trajectories; the slip ...
Alaniz-Álvarez, Susana A. +2 more
core
Evidence for surface uplift of the Atlas Mountains and the surrounding peripheral plateaux: Combining apatite fission-track results and geomorphic indicators in the Western Moroccan Meseta (coastal Variscan Paleozoic basement) [PDF]
, 2010 This work represents an initial attempt to link the evolution of the topography in relation to the general tectonic framework of western Morocco. For this purpose, in a section of the Western Moroccan Meseta different tools are combined in order to ...
A. Azdimousa +58 more
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The influence of Cenozoic Eurasia-Arabia convergence on the Southeast Arabian Foreland Basin: new geochronological and geochemical constraints from syn-kinematic carbonate mineralization. [PDF]
Sci Rep, 2023 Arboit F +5 more
europepmc +1 more source
Extensional neotectonics around the bend of the Western/Central Alps: an overview [PDF]
, 2018 The Western Alps' active tectonics is characterized by ongoing widespread extension in the highest parts of the belt and transpressive/compressive tectonics along its borders.
Allanic, Cécile +5 more
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The relationship between the plutonic intrusions and the dyke swarm in the Los Pedroches batholith (Iberian Massif, Spain): Dykes as a paleotectonic and paleostress indicators [PDF]
, 1997 [Abstract] The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large biotite ±amphibole granodiorite pluton and several, smaller variable porphyritic, biotite ± cordierite granite intrusions.
Alonso Olazábal, A. +3 more
core +1 more source
Active strike-slip faulting in the Chablais area (NW Alps) from earthquake focal mechanisms and relative locations [PDF]
, 2018 .: The Chablais area is characterized by a complex geological setting, resulting from the transport of nappes of various internal origins (the Prealpine nappes), thrusted in Oligocene times onto the Helvetic cover of the external zones of the Alps. While
Burkhard, Martin +5 more
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Anais da Academia Brasileira de Ciências, 2012 In Eastern South America, a series of fault-bounded sedimentary basins that crop out from Southern Uruguay to Southeastern Brazil were formed after the main collisional deformation of the Brasiliano Orogeny and record the tectonic events that affected ...
Renato P. Almeida +4 more
doaj
Constraining the tectonic evolution of rifted continental margins by U-Pb calcite dating. [PDF]
Sci Rep, 2023 Hestnes Å +7 more
europepmc +1 more source
Mesoproterozoic Strike-Slip Faulting within the Åland Rapakivi Batholith, Southwestern Finland
TektonikaPaleostress inversion analysis of outcrop data from brittle fault structures within the Mesoproterozoic 1.58 Ga Åland rapakivi granite, southwestern Finland, revealed two separate strike-slip faulting stages. Stage 1 is dominated by dextral slip along E–
Nicklas Nordbäck +5 more
doaj +1 more source