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Akademický článek

Transient high-level expression of ß-galactosidase after transfection of fibroblasts from GM1 gangliosidosis patients with plasmid DNA

Autor: R.C. Balestrin, G. Baldo, M.B. Vieira, R. Sano, J.C. Coelho, R. Giugliani, U. Matte

Publikováno v: Brazilian Journal of Medical and Biological Research, Vol 41, Iss 4, Pp 283-288 (2008)

GM1 gangliosidosis is an autosomal recessive disorder caused by the deficiency of lysosomal acid hydrolase ß-galactosidase (ß-Gal). It is one of the most frequent lysosomal storage disorders in Brazil, with an estimated frequency of 1:17,000. The e

Externí odkaz: https://doaj.org/article/358f95a466a2477285cbd54efbaeb024

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Silurian inverted Barrovian-type metamorphism in the Western Sierras Pampeanas (Argentina): a case of top to bottom heating?

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

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Akademický článek

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The Maz Metasedimentary Series (Western Sierras Pampeanas, Argentina). A relict basin of the Columbia supercontinent?

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

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Akademický článek

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The Faja Eruptiva of the Eastern Puna and the Sierra de Calalaste, NW Argentina: U–Pb zircon chronology of the early Famatinan orogeny

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

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Akademický článek

Polyphase white mica growth in low-grade metapelites from La Cébila Metamorphic Complex (Famatinian Belt, Argentina): evidence from microstructural and XRD investigations Crecimiento polifásico de mica blanca en metapelitas de bajo grado del Complejo Metamórfico La Cébila (Faja Famatiniana, Argentina): evidencias a partir de investigaciones microestructurales y de DRX

Autor: Sebastián O Verdecchia, Gilda Collo, Edgardo G Baldo

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

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Los mármoles cálcicos de El Escorial (Complejo Metamórfico Cushamen, Macizo Norpatagónico): caracterización isotópica de 87Sr-86Sr y edad de sedimentación

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

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The Rinconada phase: A regional tectono-metamorphic event of Silurian age in the pre-Andean basement of Argentina

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
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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/

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