Diana Cinthia Soria-Caballero- Doctor of Philosophy
- Posdoctoral researcher at Universidad Michoacana de San Nicolás de Hidalgo
Diana Cinthia Soria-Caballero
- Doctor of Philosophy
- Posdoctoral researcher at Universidad Michoacana de San Nicolás de Hidalgo
About
14
Publications
3,470
Reads
How we measure 'reads'
A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the full-text. Learn more
74
Citations
Introduction
Current institution
Publications
Publications (14)
La región costera chiapaneca es un sitio con elevada biodiversidad cuya importancia humana y medioambiental es innegable. Históricamente, ha albergado asentamientos humanos muy importantes, pero también ha reflejado en sus depósitos sedimentarios todas las alteraciones asociadas a ellos, desde la contaminación local hasta el calentamiento climático...
La falla Cerritos pertenece a la porción oeste del Sistema de Fallas Morelia-Acambay, ubicada al suroeste de la ciudad de Morelia, en el estado de Michoacán, México; en una zona con alta densidad de fallas activas con geometrías segmentadas y arreglos en échelon, donde se han desarrollado semi-grabens y grabens de dimensiones variables e inclusive...
Las regiones tectonomagmáticas activas se caracterizan por presentar sistemas de fallamiento regionales, actividad sísmica y vulcanismo recurrente. La Región Volcánica Parícutin - Tancítaro es una zona estructuralmente compleja y con alta densidad volcánica, que se localiza en el Campo Volcánico Michoacán Guanajuato dentro del sector central del Ci...
The El Malpaso - El Salto fault is a structure with en échelon geometry, composed of six main segments which combined has a length of 28 km. This fault belongs to the western sector of the Morelia-Acambay Fault System and affects Miocene - Pleistocene volcanic deposits related to the Cuitzeo ignimbrite and El Tzirate Volcanic Complex (18 and < 1.5...
The analysis of syn-sedimentary deformations is a helpful tool for paleoenvironmental reconstructions; these structures are better preserved in fluvio-lacustrine sequences. In the Zacapu basin, lacustrine sedimentation has been active since late Pliocene until modern times. During the Holocene, the lake evolved into a wetland that was the home of t...
The Trans-Mexican Volcanic Belt is an active continental volcanic arc characterized by several arc-parallel Miocene-Holocene tectonic lake basins, such as the Cuitzeo, Zacapu, Chapala, and Zacoalco. Normal faults, and related continental seismicity shape these basins. In the central part of this volcanic arc, the Cuitzeo Lake basin presents neotect...
The La Alberca-Teremendo fault is a 26 km-long, complex fault composed of an en échelon array of short crustal fault segments, belonging to the Morelia-Acambay fault system. This fault system shows parallel scarps with morphological evidence of recent activity such as drainage alteration, maximum throws of 50 m and minimum throws of 1.4 m that disp...
The Pátzcuaro–Acambay fault system (PAFS), located in the central part of the Trans-Mexican Volcanic Belt (TMVB), is delimited by an active transtensive deformation area associated with the oblique subduction zone between the Cocos and North American plates, with a convergence speed of 55 mmyr-1 at the latitude of the state of Michoacán, Mexico. Pa...
The Morelia-Acambay fault System (MAFS), located in the central part of the Trans-Mexican Volcanic Belt (TMVB) is delimited by an active transtensive deformation zone associated with the oblique subduction zone between the Cocos and North American plates, with a convergence velocity of 55 mm/yr at the latitude of the state of Michoacán, México. Par...
El actual lago de Pátzcuaro tiene una elevación de 2035 m sobre el nivel del mar. Históricamente, ha alcanzado una elevación de 2041 m, lo cual aislaba una porción de la isla cerca de la población de Jarácuaro en la parte sureste del lago. Dos trincheras realizadas en la antigua isla revelan secuencias estratigráficas tripartitas similares. En una...
