Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/2535
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Title: Application of anisotropy of magnetic susceptibility (AMS) fabrics to determine the kinematics of active tectonics: examples from the Betic Cordillera, Spain, and the Northern Apennines, Italy
Authors: Anastasio, David J.
Pazzaglia, Frank James
Parés, Josep María
Kodama, Kenneth P.
Berti, Claudio
Fisher, James A.
Montanari, Alessandro
Carnes, Lorraine Kathryn
Issue Date: May-2021
Publisher: European Geosciences Union
Citation: Solid Earth, 2021, 12 (5), 1125-1142
Abstract: The anisotropy of magnetic susceptibility (AMS) technique provides an effective way to measure fabrics and, in the process, interpret the kinematics of actively deforming orogens. We collected rock fabric data of alluvial fan sediments surrounding the Sierra Nevada massif, Spain, and a broader range of Cenozoic sediments and rocks across the Northern Apennine foreland, Italy, to explore the deformation fabrics that contribute to the ongoing discussions of orogenic kinematics. The Sierra Nevada is a regional massif in the hinterland of the Betic Cordillera. We recovered nearly identical kinematics regardless of specimen magnetic mineralogy, structural position, crustal depth, or time. The principal elongation axes are NE–SW in agreement with mineral lineations, regional GPS geodesy, and seismicity results. The axes trends are consistent with the convergence history of the Africa–Eurasia plate boundary. In Italy, we measured AMS fabrics of specimens collected along a NE–SW corridor spanning the transition from crustal shortening to extension in the Northern Apennines. Samples have AMS fabrics compatible only with shortening in the Apennine wedge and have locked in penetrative contractional fabrics, even for those samples that were translated into the actively extending domain. In both regions, we found that specimens have a low degree of anisotropy and oblate susceptibility ellipsoids that are consistent with tectonic deformation superposed on compaction fabrics. Collectively, these studies demonstrate the novel ways that AMS can be combined with structural, seismic, and GPS geodetic data to resolve orogenic kinematics in space and time.
URI: http://hdl.handle.net/20.500.12136/2535
ISSN: 1869-9510
1869-9529
DOI: 10.5194/se-12-1125-2021
Editor version: https://doi.org/10.5194/se-12-1125-2021
Type: Article
Appears in Collections:Arqueomagnetismo
Geocronología y Geología



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