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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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Proglacial lake sediment records reveal Holocene climate changes in the Venezuelan Andes

TL;DR: In this article, lake sediment records from the Cordillera de Merida in the northern Venezuelan Andes document the history of local glacial variability and climate changes during the Holocene (w12 ka to the present).
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Lithostratigraphy of the Mérida (Wisconsinan) glaciation and Pedregal interstade, Mérida Andes, northwestern Venezuela

TL;DR: In this article, more than 40 m of sediments are exposed within a fan complex formed between lateral moraines of the adjacent Mucuchache and El Caballo valleys, and Radiocarbon dating of the peats suggests they are related to warmer periods and may tentatively correlate with small D-O events detected in the oxygen-isotope record of Greenland ice cores and North Atlantic marine sediments.
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Paleoenvironmental trends in Venezuela during the last glacial cycle

TL;DR: In this paper, the main Quaternary paleoclimatic and sea-level trends recorded in Venezuela are summarized and updated, and a paleoenvironmental framework for studies addressing biogeographical, ecological, and evolutionary topics is provided.
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The Caribbean–South American plate boundary at 65°W: Results from wide‐angle seismic data

TL;DR: In this article, the authors presented the results of the analysis of new wide-angle seismic data across the Caribbean-South American plate boundary in eastern Venezuela at about 65°W. They used a combination of first-arrival traveltime inversion and simultaneous inversion of PmP and Pn arrivals to develop a P wave velocity model of the crust and the uppermost mantle.