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Vsevolod Yutsis

Researcher at Instituto Potosino de Investigación Científica y Tecnológica

Publications -  46
Citations -  350

Vsevolod Yutsis is an academic researcher from Instituto Potosino de Investigación Científica y Tecnológica. The author has contributed to research in topics: Volcano & Earth's magnetic field. The author has an hindex of 9, co-authored 41 publications receiving 265 citations. Previous affiliations of Vsevolod Yutsis include Universidad Autónoma de Nuevo León.

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Delimitation of ground failure zones due to land subsidence using gravity data and finite element modeling in the Querétaro valley, México

TL;DR: In this article, the authors present a stress-strain approach to analyze subsidence for an unconfined aquifer of varying thickness; this is done in two steps, namely when the aquifer is in equilibrium, and when it is totally depleted.
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The Los Humeros (Mexico) geothermal field model deduced from new geophysical and geological data

TL;DR: The Los Humeros volcanic complex, a 21 × 15 km edifice nesting volcanic domes and a complex faulting structure, is located at the eastern edge of the Trans-mexican volcanic belt (TMVB) as mentioned in this paper.
Journal Article

Subduction of the Rivera plate beneath the Jalisco block as imaged by magnetotelluric data

TL;DR: In this article, two magnetotelluric profiles perpendicular to the trench provide information on the subduction of the Rivera plate under the Jalisco block (JB), and the geometry of the subducting slab is inferred by the anomalous conductor on the top of the profile in the central part of the JB.
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Contourite systems in the region of the southern São Paulo Plateau escarpment, South Atlantic

TL;DR: In this article, a high-resolution parametric echo-sounder (SES 2000 deep) was used on cruises 33, 35, and 37 of the R/V Akademik Ioffe to detect erosional-depositional contourite systems on the Sao Paulo Plateau escarpment and its toe in the South Atlantic.
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Southward Migration of Magmatic Activity in the Colima Volcanic Complex, Mexico: An Ongoing Process

TL;DR: In this article, the anomalous location of volcanism in this area originates in an anomalous subduction process of the Rivera and Cocos plates and evoke a tectonic model, proposed elsewhere, to support the idea.