Results 61 to 70 of about 3,355 (205)
Elongate summit calderas as Neogene paleostress indicators in Antarctica [PDF]
Open-File Report, 2007 The orientations and ages of elongate summit calderas on major polygenetic volcanoes were compiled to document Miocene to Pleistocene Sh (minimum horizontal stress) directions on the western and northern flanks of the West Antarctic rift system. Miocene to Pleistocene summit calderas along the western Ross Sea show relatively consistent ENE long axis ...
T.S. Paulsen, T.J. Wilson
openaire +1 more source
Tectonics, Volume 44, Issue 9, September 2025.Abstract Sant'Anna Pelago is located near the extensional front of the Northern Apennines (Italy) between Modena and Lucca, an area characterized by multiple lateral steps of the NW‐SE striking tectonic system and orographic divide. The region is affected by significant instrumental seismicity with over a thousand recorded events (0.5 < M < 4.8) from ...
S. Lenci +5 more
wiley +1 more source
Tectonics, Volume 44, Issue 9, September 2025.Abstract This study presents the first rigorous statistical analysis of the present‐day crustal stress along the western margin of the North American Plate, covering the entire Canadian Cordillera and Alaska. Using circular statistics and geometric tests, we develop a regional stress province model that constrains the directions of first‐order stresses.
T. Stephan, E. Enkelmann
wiley +1 more source
From Oblique Thrust to Strike-Slip Fault: Progressive Stages of an Accretionary Wedge Development [PDF]
LithosphereAccretionary wedges of orogenic belts develop differently based on the direction of thrusting, which can be perpendicular to oblique to the belt. In the case of oblique thrusting, stress partitioning occurs, which dissects the accretionary wedge, changes
Martin Šuťjak +13 more
doaj +1 more source
Tensorial analisis of the superposed deformation in the easthern border of the Madrid basin [PDF]
, 1994 An analysis of Neogene brittle deformation using fault populatíon analysis methods has been carried out between the SW border of the Iberian Range and Altomira Range.
González Casado, J. M. +2 more
core +1 more source
Determination of present-day stress tensor and neotectonic interval in the Spanish Central System and Madrid Basin, central Spain [PDF]
, 1996 A brittle deformation tectonic analysis was performed in central Spain (Spanish Central System and Madrid Basin) in order to decipher and understand the deformation processes that take place in a typical intracontinental zone.
Giner, Jorge +4 more
core +2 more sources
How tightly does calcite e-twin constrain stress? [PDF]
, 2015 Erratum to “How tightly does calcite e-twin constrain stress?” [J. Struct. Geol. 72 (2015) 83–95] Journal of Structural Geology, Volume 80, November 2015, Page 1 => j.jsg.2015.08.004.pdfMechanical twinning along calcite e-planes has been used for ...
Yamaji, Atsushi
core +1 more source
The paleostress history of the Central European Basin System [PDF]
, 2009 Scientific Technical Report STR ; 09 ...
openaire +4 more sources
Microstructural Evolution of Carrara Marble During Semi‐Brittle Deformation
Journal of Geophysical Research: Solid Earth, Volume 130, Issue 8, August 2025.Abstract Fifteen marble samples were subjected to semi‐brittle deformation through triaxial compression experiments, reaching axial strains of about 0.5%, 1.0%, 2.0%, 4.0%, or 7.5% at temperatures of 20°C, 200°C, or 350°C, under a confining pressure of 400 MPa.
Tongzhang Qu +3 more
wiley +1 more source
Geodinamica Acta, 2018 Cenozoic convergence, collision and subsequent subduction between African and Eurasian plates are accommodating in overriding Eurasian plate both forming the Aegean extension and the North & East Anatolian fault zones.
Ökmen Sümer +3 more
doaj +1 more source