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GeoRef Categories
Date
Availability
The Mechanisms of Tsunami Amplification and the Earthquake Source of the 2021 M 7 Acapulco, Mexico, Earthquake Available to Purchase
Surface Deformation of North‐Central Oklahoma Related to the 2016 M w 5.8 Pawnee Earthquake from SAR Interferometry Time Series Available to Purchase
Field Reconnaissance after the 25 April 2015 M 7.8 Gorkha Earthquake Available to Purchase
Assembly of a large earthquake from a complex fault system: Surface rupture kinematics of the 4 April 2010 El Mayor–Cucapah (Mexico) M w 7.2 earthquake Open Access
Fault‐Slip Source Models for the 2011 M 7.1 Van Earthquake in Turkey from SAR Interferometry, Pixel Offset Tracking, GPS, and Seismic Waveform Analysis Available to Purchase
Report on the August 2012 Brawley Earthquake Swarm in Imperial Valley, Southern California Available to Purchase
Coseismic and Postseismic Slip of the 2004 Parkfield Earthquake from Space-Geodetic Data Available to Purchase
Aseismic deformation of a fold-and-thrust belt imaged by synthetic aperture radar interferometry near Shahdad, southeast Iran Available to Purchase
Deformation during the 12 November 1999 Düzce, Turkey, Earthquake, from GPS and InSAR Data Available to Purchase
Active deformation at the boundary between the Precordillera and Sierras Pampeanas, Argentina, and comparison with ancient Rocky Mountain deformation Available to Purchase
The Precordillera and Sierras Pampeanas of western Argentina are active thin-skinned and thick-skinned deformational provinces in the foreland of the Andean orogenic system and occur above a subhorizontal segment of the subducting plate. The two morphostructural provinces are analogous to the Idaho-Wyoming thrust belt and Rocky Mountain foreland provinces, respectively, that were formed in the western United States in Late Cretaceous to early Cenozoic time. Comparisons of the younger structures at the boundary between the Precordillera and Sierras Pampeanas with analogous, more eroded, structures in North America aid in the interpretation of the subsurface structural geometry of both orogenic belts and shed some light on the factors that control the style of deformation at the contact between thin- and thick-skinned deformational provinces. The Eastern Precordillera subprovince is bordered on the east by the Sierras Pampeanas basement block-uplift province. It has been deformed in late Cenozoic to Recent time into a set of folds and thrusts that verge westward, as opposed to the eastward vergence of the structures in the adjoining Central Precordillera subprovince. While few subsurface data are available, we have interpreted this subprovince to have been deformed by a combination of basement-involved and thin-skinned structures, in a manner analogous to that of the Moxa Arch in the zone of overlap between the thin-skinned and thick-skinned thrust belts in North America. We suggest that the change in structural style between the Precordillera and the Sierras Pampeanas provinces is most likely related to paleogeographic contrasts, and that the change in vergence between the Eastern and Central Precordillera subprovinces may be due to the presence of a reactivated Paleozoic fault zone.