Zobrazeno 1 - 10
of 69
pro vyhledávání: '"Rossi, J. N."'
Autor:
Guillermo Sardi, Fernando1 fgsardi@csnat.unt.edu.ar, Marangone, Silvana1 silvana_mare@hotmail.com, Manuel Fuenlabrada, José2 jmfuenla@pdi.ucm.es
Publikováno v:
Brazilian Journal of Geology. 2021, Vol. 51 Issue 3, p1-8. 8p.
Publikováno v:
Estudios Geológicos; Vol. 66 No. 2 (2010); 157-169
Estudios Geológicos; Vol. 66 Núm. 2 (2010); 157-169
Estudios Geológicos
Consejo Superior de Investigaciones Científicas (CSIC)
Estudios Geológicos; Vol. 66 Núm. 2 (2010); 157-169
Estudios Geológicos
Consejo Superior de Investigaciones Científicas (CSIC)
The San Cristóbal pluton is a 35 km2 granitic body that outcrops at the southestern tip of the Sierra de Velasco, located west of La Rioja city, Argentina. It is formed by monzogranites and syenogranites, together with scarce granodiorites, with med
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::5823a08bf44cbf622e345f042b73c9a8
https://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/789
https://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/789
Publikováno v:
Estudios Geologicos, Vol 48, Iss 5-6, Pp 279-287 (1992)
Estudios Geológicos; Vol. 48 No. 5-6 (1992); 279-287
Estudios Geológicos; Vol. 48 Núm. 5-6 (1992); 279-287
Estudios Geológicos
Consejo Superior de Investigaciones Científicas (CSIC)
Estudios Geológicos; Vol. 48 No. 5-6 (1992); 279-287
Estudios Geológicos; Vol. 48 Núm. 5-6 (1992); 279-287
Estudios Geológicos
Consejo Superior de Investigaciones Científicas (CSIC)
In the Cordillera Oriental Argentina (22 and 26° S), the Puncoviscana Formation Basin was developed, in which an extensional tectonic setting would had been supported from Upper Precambrian to Middle Ordovician. That is suggested by the limited crus
Publikováno v:
Estudios Geologicos, Vol 48, Iss 5-6, Pp 279-287 (1992)
In the Cordillera Oriental Argentina (22 and 26° S), the Puncoviscana Formation Basin was developed, in which an extensional tectonic setting would had been supported from Upper Precambrian to Middle Ordovician. That is suggested by the limited cr
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
2 p.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4e9c25e4444541b157d374ad4acb77b4
http://hdl.handle.net/10261/32816
http://hdl.handle.net/10261/32816
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
2 p.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e95fb6a1ddec385d433168bd0b0bb431
http://hdl.handle.net/10261/32717
http://hdl.handle.net/10261/32717
Autor:
Aceñolaza, Pablo G., Toselli, A. J., Saavedra Alonso, Julio, Rossi, J. N., Pellitero Pascual, E.
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Symposium International "Géodynamique Andine", Grenoble (FRA), 1990/05/15-17
At las Planchadas there is a slightly alkaline to subalkaline volcanism affected by a low grade metamorphism with features indicating continental proximity and a subaq
At las Planchadas there is a slightly alkaline to subalkaline volcanism affected by a low grade metamorphism with features indicating continental proximity and a subaq
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::19c06a2a2503d6dfe50bc33aa1db52e3
http://www.documentation.ird.fr/hor/fdi:31072
http://www.documentation.ird.fr/hor/fdi:31072
Akademický článek
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Akademický článek
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Publikováno v:
Geological Society, London, Special Publications; 2011, Vol. 350 Issue: 1 p175-186, 12p