Zobrazeno 1 - 10
of 54
pro vyhledávání: '"Carlos Oscar Limarino"'
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
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
Autor:
Carlos Oscar Limarino, Leonardo R. Scarlatta, Patricia L. Ciccioli, Sabrina Miyno, Fanny Bello, Silvia N. Césari
Publikováno v:
Andean Geology. 50:127
The La Veteada Formation, in the Sierra de Famatina (west of Argentina), is one of the few records of Early Triassic age in South America verified by isotopic age and palynological assemblages. This unit is composed of sandstones, mudstones, shales,
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)
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
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062020000200275
Autor:
Peter Zabala Medina, Néstor Bonomo, Ana Osella, Salomé Salvó Bernárdez, Carlos Oscar Limarino
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
This paper deals with the application of the Ground Penetrating Radar (GPR) method and the analysis of attributes of the GPR data to characterize and interpret a fluvial-aeolian interaction field located in the Guandacol Valley, northwest Argentina.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::630cfd0d65b9a6861b0867d5a1c9fde0
https://www.sciencedirect.com/science/article/abs/pii/S0895981119303864
https://www.sciencedirect.com/science/article/abs/pii/S0895981119303864
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
Publikováno v:
Journal of South American Earth Sciences. 84:127-148
Both global and regional climate drivers contributed to glaciation during the late Paleozoic Ice Age (LPIA). However, the transition from icehouse to greenhouse conditions was asynchronous across Gondwana suggesting that, in some cases, regional cont
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
Autor:
Sergio A. Marenssi, Carlos Oscar Limarino, Patricia Lucia Ciccioli, Richard M. Friedman, Silvia N. Césari
Publikováno v:
Journal of South American Earth Sciences. 112:103531
This paper examines the relationship between the sedimentation in the retroarc Paganzo Basin and the activity of the magmatic arc developed in the neighboring Andean Cordillera during the Late Pennsylvanian-Cisuralian. The temporal relationships betw
Publikováno v:
Marine and Petroleum Geology. 88:907-931
This paper analyses the diagenetic evolution of sandstones belonging to the Bajo Barreal Formation (Cretaceous) in the Golfo de San Jorge Basin (Patagonia, Argentina). The Bajo Barreal Formation includes the main reservoirs, which are located along t