Zobrazeno 1 - 10
of 54
pro vyhledávání: '"Elena Centeno García"'
Autor:
Gilberto Silva-Romo, Claudia Cristina Mendoza-Rosales, Emiliano Campos-Madrigal, Elena Centeno-García, Orestes Antonio de la Rosa-Mora
Publikováno v:
Journal of Maps, Vol 16, Iss 2, Pp 17-27 (2020)
This work offers a large-scale approach to the stratigraphy of an area in southern Mexico that includes three different tectono-stratigraphic terranes and displays a great geological diversity. In the attached 1:100,000-scale geological map, the stra
Externí odkaz:
https://doaj.org/article/f654ab69ffbd4ea893c0be9a3ea48c8a
Autor:
Glendy Jezabel León‐García, Agustín Gómez‐Álvarez, Diana María Meza‐Figueroa, Jesús Leobardo Valenzuela‐García, Martín Antonio Encinas‐Romero, Arturo Israel Villalba‐Atondo, Elena Centeno‐García, Kareen Krizzan Encinas‐Soto
Publikováno v:
Environmental Progress & Sustainable Energy.
Autor:
Elena Centeno-García, Gilberto Silva-Romo, Sandra Guerrero-Moreno, Berlaine Ortega-Flores, Luigi Solari, Vanessa Colás, Manuel Grajales-Nishimura, Michelangelo Martini
Publikováno v:
International Geology Review. 62:421-427
The origin of the Oligocene turbidites from the Cerro Pelon area in south Gulf Mexico proposed by Ortega-Flores et al. (2018) is in disagree with the interpretations made by Molina-Garza et...
Autor:
Francisco Martín Romero, Elena Centeno-García, Mary Kay O'Rourke, Marco Antonio Martínez-Cinco, José Leopoldo Mendoza-Lagunas, Maria Mercedes Meza-Montenegro, Diana Meza-Figueroa, Leticia García-Rico
Publikováno v:
Journal of Geoscience and Environment Protection. :90-105
A highly acidic spill from one of the most important copper mines in the Americas (Buenavista del Cobre) occurred in Sonora, Mexico in August, 2014. 40,000 m3 of metals-enriched sulphate solution escaped into the Sonora River representing the worst e
Autor:
Elena Centeno-García, Joaquín A. Proenza, William L. Griffin, Takako Satsukawa, Suzanne Y. O'Reilly, Cristina Talavera, Elena Belousova, Antonio García-Casco, Antoni Camprubí, Vanessa Colás, José María González-Jiménez, Júlia Farré-de-Pablo
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Rufino Lozano-Santa Cruz, Arturo Joaquín Barrón-Díaz, Elena Centeno-García, Margarita López-Martínez, Saúl Herrera-Urbina, Francisco A. Paz-Moreno
Publikováno v:
International Geology Review. 61:1189-1206
Volcaniclastic units are exposed at the base of the Puerto Blanco Formation in the Caborca region, northwestern Mexico. The lower unit reveals the presence of Early Cambrian mafic volcanism in this...
Autor:
Manuel Grajales-Nishimura, Sandra Guerrero-Moreno, Gilberto Silva-Romo, Vanessa Colás, Luigi Solari, Michelangelo Martini, Berlaine Ortega-Flores, Elena Centeno-García
Publikováno v:
International Geology Review. 61:915-935
In southeastern Mexico, Jurassic and Cretaceous rocks are buried beneath voluminous Palaeogenesedimentary successions, the origin of which is still under debate. Some authors proposed that ...
Autor:
J.M. Grajales-Nishimura, Luigi Solari, Ricardo Torres-Vargas, Peter Schaaf, Gustavo Murillo-Muñetón, M.A. Ramos-Arias, Elena Centeno-García
Publikováno v:
International Journal of Earth Sciences. 107:1005-1031
The Juchatengo complex (JC) suite is located between the Proterozoic Oaxacan complex to the north and the Xolapa complex to the south, and was amalgamated by late Paleozoic magmatism. It consists of mafic and sedimentary rocks that have oceanic affin
Autor:
Elena Centeno-García, William L. Griffin, José María González-Jiménez, Vanessa Colás, Antoni Camprubí, Suzanne Y. O'Reilly, Júlia Farré-de-Pablo, Takako Satsukawa, Antonio García-Casco, Elena Belousova, Cristina Talavera, Joaquín A. Proenza
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite, Baja California Sur State, Mexico. These are high-Cr chromitites [Cr# (Cr/Cr + Al atomic ratio = 0.61-0.69)] that contain a range of minor- and trace-elemen
Autor:
Elena Centeno-García
Publikováno v:
Ore Geology Reviews. 81:1035-1052
The Geological Framework of Mexico is formed by a mosaic of tectono-stratigraphic terranes that were assembled during the Paleozoic and Mesozoic as the result of the complex interaction between Laurentia, Gondwana, and the paleo-Pacific plate. Even t