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Maximiliano Bezada

Researcher at University of Minnesota

Publications -  79
Citations -  1586

Maximiliano Bezada is an academic researcher from University of Minnesota. The author has contributed to research in topics: Lithosphere & Subduction. The author has an hindex of 21, co-authored 72 publications receiving 1302 citations. Previous affiliations of Maximiliano Bezada include University of Oregon & Universidad Pedagógica Experimental Libertador.

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Evidence for slab rollback in westernmost Mediterranean from improved upper mantle imaging

TL;DR: In this paper, the deployment and data processing for Spanish stations was funded by Consolider-Ingenio 2010 project TOPO-IBERIA (CSD2006-00041) as well as ALERT-ES (CGL2010-19803-C03-02).
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Solar modulation of Little Ice Age climate in the tropical Andes

TL;DR: A 1,500-year reconstruction of climate history and glaciation in the Venezuelan Andes using lake sediments highlights the sensitivity of high-altitude tropical regions to relatively small changes in radiative forcing, implying even greater probable responses to future anthropogenic forcing.
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Receiver function study of the crustal structure of the southeastern Caribbean plate boundary and Venezuela

TL;DR: In this article, the authors used the primary P-to-S conversion and crustal reverberations to estimate crustal thickness and average crustal VP/VS ratio over the southeastern Caribbean plate boundary with the receiver function technique.
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Subduction-driven recycling of continental margin lithosphere

TL;DR: In this article, the authors show that the bottom of the continental thermal boundary layer can be removed from adjacent continental margins, leading to the loss of continental lithosphere adjacent to a subduction zone.
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Abrupt Younger Dryas cooling in the northern tropics recorded in lake sediments from the Venezuelan Andes

TL;DR: A radiocarbon dated sediment record from Laguna de Los Anteojos, a cirque lake in the Merida Andes of Venezuela, indicates that warmer and wetter atmospheric conditions occurred in the northern tropics at the onset of the Bolling (∼ 14,600 cal yr BP), and abruptly colder and drier conditions around the time of the Younger Dryas (YD) as mentioned in this paper.