Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Gonzalo Galaz"'
Autor:
Alexis Ordaz Hernández, José Ramón Hernández Santana, Carlos Enrique Cofiño Arada, Ana Patricia Méndez Linares, Gonzalo Galaz Escanilla
Publikováno v:
Investigaciones Geográficas, Iss 82, Pp 7-23 (2013)
La investigación se enfoca en revelar las princi- pales expresiones morfotectónicas del relieve, como contri- bución al estudio de la sismicidad moderada del territorio. El análisis morfoestructural se combina con resultados del análisis de estr
Externí odkaz:
https://doaj.org/article/94185bc367774f0389f17ba4a3158ee5
Autor:
Alexis Ordaz Hernández, José Ramón Hernández Santana, Carlos Enrique Confiño Arada, Ana Patricia Méndez Linares, Gonzalo Galaz Escanilla
Publikováno v:
Investigaciones Geográficas, Vol 0, Iss 82 (2013)
The research focuses on revealing the main morphotectonic expressions of relief, as a contribution to the study of moderate seismicity of territory. Morphostructural analysis combined with results of analysis of structures, to mesoscopic scale, provi
Externí odkaz:
https://doaj.org/article/404e5abec9f44bfda5474c7c2a608b0c
Autor:
Mauricio Calderon, Francisco Hervé, Rodrigo Javier Suárez, Diego Rojo, Thomas Theye, Gonzalo Galaz, Catalina Zúñiga
The Cordillera de Darwin Metamorphic Complex (CDMC) comprise metamorphosed supracrustal rocks and metaplutonic suites which records a unique tectonic evolution among the metamorphic complexes of the southernmost Andes. The pressure (P) and temperatur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::211f5d36f6875ceaef7aa76648ccfb4c
https://doi.org/10.5194/egusphere-egu21-5612
https://doi.org/10.5194/egusphere-egu21-5612
Autor:
Gemma Acosta, Ariel Almendral, Orlando Álvarez, Inés Aramendía, María Alejandra Arecco, Juan P. Ariza, C. Arriagada, Pedro Arriola, Pilar Ávila, Patrice Baby, Vanesa Barberón, Stéphanie Brichau, Ysabel Calderon, Mauricio Calderón, Gabriela Beatriz Franco Camelio, Horacio N. Canelo, Victor Carlotto, Barbara Carrapa, Ryan Cochrane, Gilda Collo, Eduardo Contreras-Reyes, Peter Copeland, Christian Creixell, Edward Cuipa, Federico M. Dávila, Peter G. DeCelles, Juan Díaz-Alvarado, A. Echaurren, Sebastián Echeverri, A. Encinas, Adrien Eude, Miguel Ezpeleta, Lucía Fernández Paz, D. Figueroa, Andrés Folguera, Gonzalo Galaz, Héctor P.A. García, Carmala N. Garzione, Sarah W.M. George, Matías C. Ghiglione, P. Giampaoli, Guido M. Gianni, Mario Gimenez, Johannes Glodny, E. Gobbo, Marcelo A. Gonzalez, E. Gabriela Gutiérrez, Camilo Higuera, Brian K. Horton, Sofía Iannelli, Lily J. Jackson, James N. Kellogg, Keith A. Klepeis, Federico Lince Klinger, Cullen Kortyna, Thomas J. Lapen, F. Lince-Klinger, Vanesa D. Litvak, C. López, Melanie Louterbach, Leonard Luzieux, Federico Martina, Myriam P. Martinez, F. Martínez, Joseph Martinod, Ezequiel García Morabito, Héctor Mora-Páez, Federico Moreno, Francisco Sánchez Nassif, C. Navarrete, Julieta C. Nóbile, Paul O’Sullivan, Soty Odoh, Verónica Oliveros, G. Olivieri, Sebastián Correa Otto, Mauricio Parra, Ana María Patiño, A. Paul, Mark Pecha, Stefanie Pechuan, Agustina Pesce, Stella Poma, Alice Prudhomme, Juan Carlos Ramírez, Miguel E. Ramos, Alexandra Robert, E. Rocha, E.A. Rojas Vera, Christian Romero, Gonzalo Ronda, Marcos A. Sánchez, Joel E. Saylor, Edward R. Sobel, Santiago R. Soler, Richard A. Spikings, Rodrigo J. Suárez, Christian Sue, Kurt Sundell, Tonny B. Thomsen, Jonathan Tobal, Cristian Vallejo, Roelant Van der Lelij, D. Villagomez, Laura E. Webb, Wilfried Winkler, Gonzalo Zamora
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69c2b013cb5f2961a9d001fa244175ec
https://doi.org/10.1016/b978-0-12-816009-1.09992-5
https://doi.org/10.1016/b978-0-12-816009-1.09992-5
The metamorphic formations that outcrop along the northern and central Chilean coast (26°–39°S) represent the late Paleozoic accretionary complex at the convergent southwestern margin of Gondwana. The characteristics of the HP-LT basal units (Wes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b74460ffa16ea085742218070cf9e7ee
https://doi.org/10.1016/b978-0-12-816009-1.00017-4
https://doi.org/10.1016/b978-0-12-816009-1.00017-4
Publikováno v:
International Geology Review. 55:1401-1417
The high-pressure (HP) Piaxtla Suite at Tehuitzingo contains peridotites, gabbros, and serpentinized peridotites, as well as granitoids and metasedimentary rocks. The HP mafic rocks are characterized by low SiO2 (38–52 wt.%) and high Mg# (∼48–7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b053b42c8b66ede9673da03891550f7
https://doi.org/10.1080/00206814.2013.776806
https://doi.org/10.1080/00206814.2013.776806
Publikováno v:
Gondwana Research. 23:641-660
High-pressure (HP) rocks at Tehuitzingo, on the western margin of the HP belt within the Paleozoic Acatlan Complex (southern Mexico), occur in a klippe that was thrust over low-grade clastic rocks. The youngest detrital zircon cluster in the low-grad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d8378ddb4baecbc9c25ea4faa629f0e
https://doi.org/10.1016/j.gr.2012.04.011
https://doi.org/10.1016/j.gr.2012.04.011
Autor:
Gonzalo Galaz, Julie C. Fosdick, Francisco Fuentes, Fernando A. Sepúlveda, Mauricio Calderón, Francisco Hervé
Publikováno v:
Geodynamic Evolution of the Southernmost Andes ISBN: 9783319397252
The petrology and geochronology of Paleozoic and Mesozoic metamorphic and ophiolitic complexes in southern Patagonia constrain the evolution of magmatic belts, marginal basins, and continental fragments that once formed part of the peripheral realm o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::532ebcf2bd5636eec60b26007f56ddfe
https://doi.org/10.1007/978-3-319-39727-6_2
https://doi.org/10.1007/978-3-319-39727-6_2
Autor:
Gonzalo Galaz-Escanilla, J. Brendan Murphy, Jaroslav Dostal, M.A. Ramos-Arias, R. Damian Nance, J. Duncan Keppie
Publikováno v:
Tectonophysics. :1-21
High pressure (HP) rocks in the Paleozoic Acatlan Complex of southern Mexico occur in a median belt extruded into the complex, which is the root zone of a klippe to the west. These HP rocks are predominantly clastic metasedimentary rocks and include
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36660e49d21fb42620e745d7e92fb0a5
https://doi.org/10.1016/j.tecto.2012.06.015
https://doi.org/10.1016/j.tecto.2012.06.015
Autor:
Mauricio Calderón, Christopher Fanning, Gonzalo Galaz, Clare J. Warren, Francisco Hervé, James Schwanethal, L. Fadel Cury, Hans-Joachim Massonne, D. Gaytan, Paulo E. Fonseca, Julie C. Fosdick
Publikováno v:
TECTONOPHYSICS
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The Canal de las Montanas Shear Zone (CMSZ), southern Patagonian Andes (51–52°S), is a low-grade mylonite belt generated from felsic ignimbritic, pelitic and basaltic protoliths of the Late Jurassic–Early Cretaceous Rocas Verdes basin. The diffe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3910df5213e3dcd14d1e6ee48a6142b9
https://doi.org/10.1016/j.tecto.2011.12.034
https://doi.org/10.1016/j.tecto.2011.12.034