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

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2504-3625 contributed to the collection..Studies illustrate the vast .Geodynamics of the Latin American Pacific Margin presents a collection of 22 studies by a multinational group of investigators whose common interest is to better understand the complex geodynamic processes occurring along the Pacific margi

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,Low Angle Contact Between the Oaxaca and Juárez Terranes Deduced From Magnetotelluric Data,forces may contribute to uplift because it is largely uncompensated. In the Sierra Madre del Sur, closer to the coast, uplift is facilitated by slab-dehydration driven buoyancy. Both gravity and resistivity models are consistent with a thinned upper crust in the northeast end of the profile.

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P. H?lemann,R. Hasselmann,G. Dixerprint and amphibolite-eclogite transition, respectively. (4) The evidences that document ridge-jump events and associated microplate individualization during subduction of the SCR1 and SCR-1 segments: the Chonos and Cabo Elena microplates, respectively. The ridge-jump process associated with the o

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Textilforschungsanstalt Krefeldomains. The pattern recognition in one domain was independent of the pattern recognition in another domain. We found and verified with two independent catalogue data sets (CSN, IPOC) that within a critical area of ca. 65?km from the main shock epicenter, the 2014 event was preceded by distinct fores

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https://doi.org/10.1007/978-3-0348-4170-2trikes and source geometries indicate an emplacement of intrusive bodies controlled by the regional faults affecting the Auca Mahuida basement and the sedimentary successions of the Neuquén basin. Magma upraised along these faults and fractures feeding the volcanic activity and subsequently crystall

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