La sucesión carbonífera de la Quebrada Agua de la Peña (Sierra De Valle Fértil): ambientes sedimentarios, contenido fosilífero e importancia estratigráfica.

Autor: Carina Ester Colombi, Carlos Oscar Limarino, Silvia Nélida Césari

Publikováno v: Latin American Journal of Sedimentology and Basin Analysis, Vol 25, Iss 1 (2021)

La Formación Tuminico, en el área de la quebrada Agua de la Peña, forma una sucesión de 1128 m de espesor, la que caracteriza la sedimentación carbonífera tardía, aflorante próxima al lineamiento de Valle Fértil. La unidad, depositada en amb

Externí odkaz: https://doaj.org/article/48f96aee041f45aa9d52ece5a73c209c

High-precision U-Pb CA-ID-TIMS calibration of the Permian Lueckisporites-dominated assemblages in westernmost Gondwana: inferences for correlations

Autor: Fanny C. Bello, Silvia N. Césari, Richard M. Friedman, Sergio A. Marenssi, Carlos Oscar Limarino, Patricia Lucia Ciccioli, Leonardo R. Scarlatta, Luís Carlos de Souza Ferreira

Publikováno v: Palynology. 46:1-20

Palynology is one of the most useful tools for constructing biostratigraphic charts in the late Paleozoic basins of South America, but the lack of radiometric ages often makes it difficult to establish the precise age of the biozones. This paper focu

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e44ed7f0fa57acaa4cc61d83edbd528e
https://doi.org/10.1080/01916122.2021.1968060

Microfábricas pedogénicas y de exposición subaérea en el sistema volcánico y lacustre de la formación san ignacio (Carbonífero Superior-Pérmico Inferior), Cordillera Frontal, Argentina

Autor: I. Méndez-Bedia, Eva Prats, Raúl Cardó, Gloria Gallastegui, Carlos Oscar Limarino, Ferran Colombo, P. Busquets, Silvia N. Césari

Publikováno v: Andean geology v.47 n.2 2020
SciELO Chile
CONICYT Chile
instacron:CONICYT
WOS:000542682600003
RUO. Repositorio Institucional de la Universidad de Oviedo
Universidad de las Islas Baleares
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)

In the Argentinian Andes (Frontal Cordillera) the upper part of the late Carboniferous-early Permian San Ignacio Formation is made up of lacustrine-palustrine microbial carbonates and interbedded volcanic deposits. In this lacustrine-palustrine envir

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4a06923d6eb13c74685cee483cce4779
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062020000200275

Fluvial-aeolian interaction deposits in the Andean Foreland basin (Northwest Argentina): Architecture and facies model

Autor: Néstor Bonomo, Ana Osella, Salomé Salvó Bernárdez, Peter Zabala Medina, Carlos Oscar Limarino

Publikováno v: Aeolian Research. 54:100754

The fluvial-aeolian interaction field of the Guandacol valley (northwest Argentina) is studied through different methodologies that comprise satellite, drone and GPR images, bedform descriptions, and grain-size analysis. The obtained information allo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::aac499e122b2988e051293cc966f30b2
https://doi.org/10.1016/j.aeolia.2021.100754

Depositional settings and evolution of a fjord system during the carboniferous glaciation in Northwest Argentina

Autor: Carlos Oscar Limarino, Ferrán Colombo Piñol, Pablo J. Alonso-Muruaga, Luis Antonio Spalletti

Publikováno v: Sedimentary Geology. 369:28-45

Fjord systems, represented by glacial diamictites and postglacial transgressive shales, formed in the basins of western Argentina during the late Carboniferous Gondwana glaciation. Well exposed fjord deposits of the Guandacol Formation were studied i

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9ec266221ae878366017bff0595ebfc3
https://doi.org/10.1016/j.sedgeo.2018.03.002