Titlebook: Geodynamics of the Latin American Pacific Margin; William L. Bandy,Juanjo Dañobeitia,Rafael Bartolom Book Feb 20171st edition Springer Int

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Foreshock Patterns Preceding Great Earthquakes in the Subduction Zone of Chile,al foreshock sequences has shown that foreshocks are characterized by distinct 3D patterns: their epicenters move towards the main shock epicenter, event count accelerates, and .-value drops. However, these space–time-size patterns were verified so far only in a very few individual cases mainly due

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Analysis of the Aeromagnetic Anomalies of the Auca Mahuida Volcano, Patagonia, Argentina,le geological information. Most of the detected magnetic anomalies have a dipolar structure opposite to that of the present geomagnetic field. According to the available geochronological data and paleomagnetic measurements, the source bodies of Auca Mahuida mainly emplaced in the Matuyama reverse po

针叶

Ibd810

conjunctivitis

Three-Dimensional Thermal Model of the Costa Rica-Nicaragua Subduction Zone,uake seismogenic zone and volcanic arc magmatism. Here, we present the first three-dimensional (3D), steady-state kinematic-dynamic thermal model for the Costa Rica-Nicaragua subduction zone. The model consists of the subducting Cocos plate, the overriding Caribbean Plate, and a viscous mantle wedge

conjunctivitis

,Kinematic 3-D Retro-Modeling of an Orogenic Bend in the South Limón Fold-and-Thrust Belt, Eastern Cnes and is therefore a natural laboratory for the analysis of curved orogens. The analysis of curved fold-and-thrust belts is a challenge because of the varying structural orientations within the belt. Based on seismic reflection lines, we created a 3-D subsurface model containing three major thrust

描述

,Low Angle Contact Between the Oaxaca and Juárez Terranes Deduced From Magnetotelluric Data,cognized tectonic features at upper to mid-crustal depths. Our results support the hypotheses that the upper crust of the Oaxaca terrane is a residual ~20 km thick crust composed by an ~10 km thick faulted crustal upper layer and an ~10 km thick hydrated and/or mineralized layer. Oaxaca basement ove

陶器

Seismic Anisotropy and Mantle Flow Driven by the Cocos Slab Under Southern Mexico,rn Mexico starting at the coast of the Pacific Ocean and running north toward the Gulf of Mexico. In this segment of the Middle America Trench the oceanic Cocos plate subducts under the continental North American plate. The active volcanic arc is located at the southern end of the Trans-Mexican Volc

Thymus

Toroidal, Counter-Toroidal, and Upwelling Flow in the Mantle Wedge of the Rivera and Cocos Plates: bduction zone. The scaled model consists of a transparent tank filled with corn syrup and housing two conveyor belts made of polyethylene strips. One of the strips dips 60° and moves at a velocity of 30 mm/min simulating the Rivera plate. The other one dips 45°, moves at 90 mm/min simulating the sub