Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Sebastián Rocher"'
Autor:
Juan A. Dahlquist, Matías M. Morales Cámera, Pablo H. Alasino, Robert J. Pankhurst, Carlos W. Rapela, Juan A. Moreno, Edgardo G. Baldo, Sebastián Rocher
Publikováno v:
International Geology Review. 65:489-490
Autor:
Virginia Valeria Reinoso Carbonell, Gimena Mariel Uran, Marcos Simón Macchioli Grande, Pablo H. Alasino, Mariano A. Larrovere, Sebastián Rocher, Gabriel G. Moreno
Publikováno v:
Journal of Structural Geology. 118:1-20
Detailed mapping of the Huaco intrusive Complex in NW Argentina documents a shift in the emplacement style of successive magma additions in an upper crustal environment as the system evolves thermally. The units of the Huaco intrusive complex exhibit
Autor:
Lucas E. Fiorelli, E. Martín Hechenleitner, Leonardo Salgado, Agustín G. Martinelli, Sebastián Rocher, Jeremías R. A. Taborda, Léa Leuzinger
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Communications Biology
Communications Biology, Vol 3, Iss 1, Pp 1-13 (2020)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Communications Biology
Communications Biology, Vol 3, Iss 1, Pp 1-13 (2020)
South American titanosaurians have been central to the study of the evolution of Cretaceous sauropod dinosaurs. Despite their remarkable diversity, the fragmentary condition of several taxa and the scarcity of records outside Patagonia and southweste
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b443120b2c323bee40b35ed0af03ca2a
http://www.nature.com/articles/s42003-020-01338-w
http://www.nature.com/articles/s42003-020-01338-w
Autor:
Hugo Tickyj, Matías M. Morales Cámera, Miguel Angelo Stipp Basei, Sebastián Rocher, Carmen Galindo, Juan A. Dahlquist, Pablo H. Alasino, Juan Moreno
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
Whereas north of 33°S Devonian calcalkaline magmatism is notably absent, a Devonian arc is well developed to the south of 33°S. The Carrizalito, Pampa de los Avestruces, and Papagayos plutons are l...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2f2f42089fe1632752bd2d036880a63b
Autor:
Juan Antonio Moreno, Sebastián Rocher, Matías M. Morales Cámera, Marcos Simón Macchioli Grande, Pablo H. Alasino, Mariano A. Larrovere, Juan A. Dahlquist
Publikováno v:
Tectonophysics. 816:229034
The Lower Carboniferous Guandacolinos pluton of northwestern Argentina (Western Sierras Pampeanas) preserves field, structural, and petrological evidence of sheet-like transport and assembly of granitic magmas in the upper crust. The pluton is a rela
Autor:
Miguel Angelo Stipp Basei, Mariano A. Larrovere, Sebastián Rocher, Sebastián O. Verdecchia, Gabriel G. Moreno, Pablo H. Alasino, Arne P. Willner, Camilo R. de los Hoyos, César Casquet, Maria Helena Bezerra Maia de Hollanda, Edgardo G. Baldo
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
New structural data from a mid-crustal segment in the Eastern Sierras Pampeanas, coupled with geochronological methods and P–T estimates, reveal polyphase contractional deformation and metamorphism during the Famatinian Orogeny overalongperiodoftim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::42d536c556f8be31c3d4658f51508769
Autor:
George Zandt, Sebastián Rocher, Patricia Alvarado, Jean Baptiste Ammirati, Sofía B. Pérez Lujan, Susan L. Beck
Publikováno v:
Earth and Planetary Science Letters. 450:29-39
In the flat slab region of the South Central Andes (∼31–32◦S), geological observations suggest that the regional crustal structure is inherited from the accretion of different terranes during the Ordovician. These structures were later reactiva
Autor:
Pablo H. Alasino, Sebastián Rocher, Mariano A. Larrovere, Marcos Simón Macchioli Grande, Scott R. Paterson
The Asha pluton, the oldest unit of the San Blas intrusive complex (Early Carboniferous), exhibits impressive examples of magmatic structures formed by accumulation of K-feldspar megacrysts, enclaves, and schlieren. Almost all recognized structures a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7de0db5bf0c3c29a541a9843d9e25e9d
https://www.sciencedirect.com/science/article/pii/S0191814117303073
https://www.sciencedirect.com/science/article/pii/S0191814117303073
Autor:
Lucas E. Fiorelli, E. Martín Hechenleitner, Martín D. Ezcurra, Miguel Ezpeleta, Agustín G. Martinelli, Sebastián Rocher
We describe tetrapod burrows from the uppermost Middle–lower Upper Triassic (latest Ladinian–early Carnian) Chañares Formation (Ischigualasto-Villa Unión Basin), La Rioja Province, northwestern Argentina. The burrows were found in different loc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b4f765da1459aa103e01fafcc2e2001
http://linkinghub.elsevier.com/retrieve/pii/S0031018217309963
http://linkinghub.elsevier.com/retrieve/pii/S0031018217309963
Autor:
Valbone Memeti, Sebastián Rocher, Miguel Angelo Stipp Basei, Juan A. Dahlquist, Carmen Galindo, Mariano A. Larrovere, Marcos Simón Macchioli Grande, Mario da Costa Campos Neto, Pablo H. Alasino, Scott R. Paterson
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Carboniferous igneous activity in the Sierra de Velasco (NW Argentina) led to the emplacement of several magmas bodies at shallow levels (< 2 kbar). One of these, the San Blas intrusive complex formed over millions of years (≤ 2–3 m.y.) through t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::353567410775ea52da7e23c30d14f3dd
http://hdl.handle.net/10261/185495
http://hdl.handle.net/10261/185495