Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Sebastián O Verdecchia"'
Publikováno v:
Andean Geology, Vol 38, Iss 2, Pp 268-283 (2011)
Two tectono-thermal metamorphic events, M1-D1 (S1, with associated white mica and chlorite: WM1-Chl1) and M2-D2 (S2, with development of WM2-Chl2), are established from polyphase white mica growth for low-grade units from the Ordovician metasedimenta
Externí odkaz:
https://doaj.org/article/38c76f25c852495fa7085b307db32cb1
Autor:
Sebastián O. Verdecchia, Cesar Casquet, Edgardo G. Baldo, Mariano A. Larrovere, Carlos I. Lembo Wuest, Manuela E. Benítez, Carlos D. Ramacciotti, Juan A. Murra, Robert J. Pankhurst
Publikováno v:
Geological Magazine. 160:972-992
This paper focuses on one orogenic belt that formed during the Rinconada phase on the final stage of the Famatinian orogeny, between 445 and 410 Ma, which is well exposed at Sierra de Ramaditas and neighbouring ranges in western Argentina. The Ramadi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79dde8be4aa0136576f69e6afdf2f59c
https://doi.org/10.1017/s0016756823000080
https://doi.org/10.1017/s0016756823000080
Autor:
Carlos D. Ramacciotti, Sebastián O. Verdecchia, Christopher Fanning, Robert J. Pankhurst, Juan A. Murra, Edgardo G. Baldo, César Casquet
Publikováno v:
Geological Magazine. 159:309-321
The Maz Metasedimentary Series is part of the Maz Complex that crops out in the sierras of Maz and Espinal (Western Sierras Pampeanas) and in the Sierra de Umango (Andean Frontal Cordillera), northwestern Argentina. The Maz Complex is found within a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e441ad37f2a0a6211d91748f83f68b63
https://doi.org/10.1017/s0016756821000935
https://doi.org/10.1017/s0016756821000935
Autor:
Chris Yakymchuk, Maarten A. T. M. Broekmans, Sebastián O. Verdecchia, Somayeh Rahmani Javanmard
Publikováno v:
Geological Journal. 56:3396-3414
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a54af600d4e42b63b77744cf8595fbf
https://doi.org/10.1002/gj.4135
https://doi.org/10.1002/gj.4135
Autor:
Carlos W. Rapela, Carlos D. Ramacciotti, César Casquet, Mariano A. Larrovere, Pablo H. Alasino, Robert J. Pankhurst, Juan A. Dahlquist, Clemente Recio, Edgardo G. Baldo, Carmen Galindo, Sebastián O. Verdecchia
Publikováno v:
Journal of Iberian Geology. 47:15-37
The Famatinian is a segment of the Ordovician Terra Australis accretionary orogen that stretched along the SW Margin of Gondwana from Australia to Colombia. The present knowledge of this orogenic segment still is incomplete. We present geochemistry a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a9d18f2fe0c95c6bd03899fee073cba
https://doi.org/10.1007/s41513-020-00150-z
https://doi.org/10.1007/s41513-020-00150-z
Autor:
Carmen Galindo, Sebastián O. Verdecchia, Carlos D. Ramacciotti, Edgardo G. Baldo, Juan A. Murra
Publikováno v:
Andean Geology. 49
The El Escorial marbles (Cushamen Metamorphic Complex) along with amphibolites form metamorphic septa within the permian granitoids of the Mamil Choique Formation (261-286 Ma). The metamorphism, determined in granulite facies migmatic gneisses septa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::556d5e00f458009cab9dd758caf52766
https://doi.org/10.5027/andgeov49n1-3387
https://doi.org/10.5027/andgeov49n1-3387
Autor:
Juan A. Murra, Edgardo G. Baldo, Mariano A. Larrovere, Carlos W. Rapela, César Casquet, Robert J. Pankhurst, Carlos D. Ramacciotti, Sebastián O. Verdecchia
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
instname
instname
A Silurian regional tectonometamorphic event has been widely recorded by different geochronological methods in the Sierras Pampeanas, NW Argentina and the Precordillera. It took place between ca. 445 and 420 Ma after the regional Hirnantian (late Ord
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3378fa1a2dbcca2a4f8558e11056df1b
https://eprints.ucm.es/id/eprint/68538/
https://eprints.ucm.es/id/eprint/68538/
Autor:
Sebastián O. Verdecchia, Cecilia Ayelén Wunderlin, Priscila Soledad Zandomeni, Mariano Fehrmann, Gilda Collo
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
In this work, crystallochemical indexes and geothermobarometric calculations are used together to estimate the P-T condition in low-grade metamorphic units of the San Luis Formation from Sierra de San Luis (Eastern Sierras Pampeanas of Argentina). Ph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc377f08b85dd27c03fe7d5c481b9a1b
https://doi.org/10.1016/j.lithos.2018.11.021
https://doi.org/10.1016/j.lithos.2018.11.021
Autor:
Catalina Balbis, Samanta Serra-Varela, Carlos I. Lembo Wuest, Juan Moreno, Juan A. Dahlquist, Manuela Benítez, Sebastián O. Verdecchia, Matías M. Morales Cámera, Priscila Soledad Zandomeni, Edgardo G. Baldo
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Minerals, Vol 11, Iss 166, p 166 (2021)
Minerals
Volume 11
Issue 2
Universidad Nacional de La Plata
instacron:UNLP
Minerals, Vol 11, Iss 166, p 166 (2021)
Minerals
Volume 11
Issue 2
The Sierra de Guasayán (Eastern Sierras Pampeanas, Argentina) is formed by low to medium grade metamorphic rocks intruded by Cambrian metaluminous (La Soledad quartz-diorite), slightly peraluminous (Guasayán, El Escondido and El Martirizado granodi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::520338c7d9951cd967aa529ff558bd0a
http://sedici.unlp.edu.ar/handle/10915/125399
http://sedici.unlp.edu.ar/handle/10915/125399