Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Matías Peña"'
Publikováno v:
Intervención, Vol 14, Iss 1 (2024)
El presente artículo tiene como objetivo observar -desde una mirada sistémica a la intervención- la relación entre las características de la violencia en el pololeo que identifican juventudes de la ciudad de Puerto Aysén y la oferta estatal par
Externí odkaz:
https://doaj.org/article/8d29cfd73e1a43178b66e4d36e7cded0
Autor:
Diana Comte, Gisella Palma, Jimena Vargas, Daniela Calle-Gardella, Matías Peña, Sergio García-Fierro, Joëlle D’Andres, Steven Roecker, Sergio Pichott
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-13 (2023)
Abstract An essential part of the world's remaining mineral resources is expected to reside deep in the crust or under post-mineralization cover. For porphyry copper deposits, the world’s primary source of Cu, Mo, and Re, identifying the dynamic pr
Externí odkaz:
https://doaj.org/article/e875f3ac0b314aadac08a2b6a9332a30
Publikováno v:
Andean Geology, Vol 39, Iss 2, Pp 258-278 (2012)
The Triassic and Jurassic tectonic history of northern Chile has been dominated by extension, although clear evidence about the nature and geometry of the extensional basins and subsequent inversion structures has been adequately illustrated in only
Externí odkaz:
https://doaj.org/article/3d7f3e09c89942c79cebde98d3c1b98b
Publikováno v:
Andean Geology, Vol 39, Iss 2, Pp 295-316 (2012)
Regional and local strike-slip systems in Chile are complex and pose interesting questions, such as the interaction between strike-slip and reverse faults, how they evolve, and the relationship between shortening, rotation and uplift. Within this con
Externí odkaz:
https://doaj.org/article/5538d940e7eb4a77b1f36aebe02e714c
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c16ec1db569da8d5e421618adc866ae2
https://doi.org/10.1111/bre.12580
https://doi.org/10.1111/bre.12580
Autor:
Fernando Poblete, S. Perroud, Fernando Martínez, Laura Giambiagi, José Mescua, Julieta Suriano, Matías Peña, Andrés Echaurren, Daniela Espinoza, I. Gómez, R. Quiroga
Publikováno v:
Journal of South American Earth Sciences. 106:102981
We present an integrated structural and Anisotropy of Magnetic Susceptibility (AMS) study focused on the characterization of the spatio-temporal variation of the strain field during the main Neogene deformation, of the Argentine Precordillera and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa6c22b8f22754064bb20a17fc13fbcd
https://doi.org/10.1016/j.jsames.2020.102981
https://doi.org/10.1016/j.jsames.2020.102981
Publikováno v:
Tectonophysics. 667:144-162
The Andean orogenic belt, located in the Central Andes “Pampean flat-slab” segment in northern Chile (27–29°S), is composed of two major tectonic regions: the Coastal Cordillera and the Frontal Cordillera. To understand their internal tectonic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::538c69609d7be73368589d763e59310e
https://doi.org/10.1016/j.tecto.2015.11.019
https://doi.org/10.1016/j.tecto.2015.11.019
Publikováno v:
Journal of South American Earth Sciences. 64:307-324
The structure of the Chilean Frontal Cordillera, located over the Central Andes flat-slab subduction segment (27°–28.5°S), is characterized by a thick-skinned deformation, affecting both the pre-rift basement and the Mesozoic and Cenozoic infill
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::73b82329fa57d593369602ac628dc2b0
https://doi.org/10.1016/j.jsames.2015.05.001
https://doi.org/10.1016/j.jsames.2015.05.001
Autor:
Andrés Mora, Fernando Martínez, Sebastián Bascuñán, César Arriagada, Mauricio Parra, Matías Peña
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Frontal Cordillera in northern Chile is located over the flat-slab subduction segment of the Central Andes. This tectonic province is characterized by a thick-skinned structural style showing evidence of tectonic inversion and basement-involved c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::837ddc7f8ae8e18ef3b0b227311aec0e
Publikováno v:
ANDEAN GEOLOGY
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Andean Geology
Andean geology v.39 n.2 2012
SciELO Chile
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Andean Geology
Andean geology v.39 n.2 2012
SciELO Chile
The Triassic and Jurassic tectonic history of northern Chile has been dominated by extension, although clear evidence about the nature and geometry of the extensional basins and subsequent inversion structures has been adequately illustrated in only
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c406a4f463cc4f41d0643c101fc60ef4