Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Estanislao Godoy"'
Publikováno v:
Andean Geology, Vol 39, Iss 3, Pp 394-406 (2012)
Las avalanchas de detritos, asociadas a colapsos parciales de edificios volcánicos, son fenómenos comunes en la evolución de un volcán. Este tipo de flujos son por inestabilidades, que pueden deberse a factores tales como la existencia de zonas a
Externí odkaz:
https://doaj.org/article/199b1e4bae374185948c1b87e9791c6b
Publikováno v:
Andean Geology, Vol 37, Iss 2, Pp 413-432 (2010)
On the west coast of Tierra del Fuego, south of Cabo Nariz, in Chile, Upper Cretaceous to Paleocene sedimentary successions of the Magallanes foreland basin crop out. The presence of dinoflagellate cysts, as well as radiometric U-Pb SHPJMP dating of
Externí odkaz:
https://doaj.org/article/926db681282a42a6b1d028d28502bf06
Publikováno v:
Andean Geology, Vol 37, Iss 1, Pp 1-31 (2010)
Four Middle-to-Late Miocene barren plutonic complexes that occur between the giant porphyry copper deposits of the central Chilean Andes were selected for U-Pb LA-ICPMS geochronology and Hf-isotope systematics on single zircon grains. Major and trace
Externí odkaz:
https://doaj.org/article/a62857bc7765459d9c9185d139b236a8
Autor:
P. Pamela Alvarez, Laura Giambiagi, José Mescua, Matías Barrionuevo, Silvana Spagnotto, Julieta Suriano, Estanislao Godoy, Ana Clara Lossada
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Geoscience Frontiers, Vol 10, Iss 6, Pp 2117-2133 (2019)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Geoscience Frontiers, Vol 10, Iss 6, Pp 2117-2133 (2019)
In this work, we develop a multidisciplinary approach to investigate a geothermal system located at the volcanic arc of a subduction-related orogen and highlight the interplay between active tectonism, stress field and fluid migration. By using resul
Autor:
C. Mark Fanning, Mauricio Calderón, Estanislao Godoy, Paulo Quezada, Rodrigo Javier Suárez, Robert J. Pankhurst, Francisco Hervé, Octavio Urbina
Publikováno v:
Andean geology v.48 n.1 2021
SciELO Chile
CONICYT Chile
instacron:CONICYT
SciELO Chile
CONICYT Chile
instacron:CONICYT
Previously undated low-grade metamorphic rocks from the Puerto Cisnes-Queulat area (44°30’ S) contain detrital zircons of mid-Oligocene age (ca. 28 Ma). Their outcrops represent the easternmost occurrence of the late Oligocene to early Miocene mar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5dd382607bb09d398a06ffe9692429a7
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062021000100054
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062021000100054
Autor:
Terence T. Kato, Estanislao Godoy
Publikováno v:
International Geology Review. 57:606-628
Melanges occur as discontinuous, mappable, units along an extensive N–S-trending, steeply dipping zone of distributed shear in metamorphic complexes along the coast of central Chile. Large melange zones, from north to south, near Chanaral, Los Vilo
Autor:
Estanislao Godoy
Publikováno v:
Geological Society, London, Special Publications. 399:155-165
Autor:
Mauricio Calderón, Francisco Hervé, Robert J. Pankhurst, Christopher Fanning, Estanislao Godoy
Publikováno v:
GONDWANA RESEARCH
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
We present detrital zircon U Pb SHRIMP age patterns for the central segment (34–42°S) of an extensive accretionary complex along coastal Chile together with ages for some relevant igneous rocks. The complex consists of a basally accreted high pres
Publikováno v:
Tectonophysics. 369:1-19
The Aconcagua fold and thrust belt, located in the Andean mountains at 32°30′ to 34°S, has been described as a classic model of a thin-skinned thrust belt. However, new structural data from its southern sector have shown that it has a complex str
Autor:
Luisa Pinto, Víctor H. García, Sebastían D. Pagano, Pamela Jara, Silvana Spagnotto, José Mescua, Hernán Porras, Andrés Tassara, Greg Hoke, Stella Maris Moreiras, P. Pamela Alvarez, Laura Giambiagi, Estanislao Godoy, Florencia Bechis, Julieta Suriano, Maisa Tunik, Felipe Tapia
Publikováno v:
RID-UNRN (UNRN)
Universidad Nacional de Río Negro
instacron:UNRN
Universidad Nacional de Río Negro
instacron:UNRN
We propose an integrated kinematic model with mechanical constrains of the Maipo-Tunuyán transect (33°40'S) across the Andes. The model describes the relation between horizontal shortening, uplift, crustal thickening and activity of the magmatic ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2547ddab58eb81d2d5bc12b50e9bef84
https://rid.unrn.edu.ar/jspui/handle/20.500.12049/5333
https://rid.unrn.edu.ar/jspui/handle/20.500.12049/5333