Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Luis Pedro Fernández"'
Autor:
Alison Campion, Adam Maloof, Blair Schoene, Sergey Oleynik, Javier Sanz‐López, Silvia Blanco‐Ferrera, Oscar Merino‐Tomé, Juan Ramón Bahamonde, Luis Pedro Fernández
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2647-2660 (2018)
Abstract During the Late Paleozoic Ice Age (LPIA, 345–260 Ma), an expansion of ice house conditions at ∼330 Ma caused a nearly synchronous, global unconformity. Subaerially exposed paleotropical carbonates were dissolved by meteoric waters, mixed
Externí odkaz:
https://doaj.org/article/b9fb2260441942cb8d1949330937cb53
Publikováno v:
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
Spanish Journal of Palaeontology, Vol 35, Iss 1, Pp 107-124 (2020)
instname
Spanish Journal of Palaeontology, Vol 35, Iss 1, Pp 107-124 (2020)
The Hoyo Oscuro section (Andara Massif, southeastern part of Picos de Europa) is a comparatively small exposure of Pennsylvanian syntectonic deposits that shown angular unconformity on the fairly extensive pre-tectonic carbonate platform strata of Pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::93f5d7eae82b901230b490e2619a1cbc
http://hdl.handle.net/10651/58055
http://hdl.handle.net/10651/58055
Autor:
M. Luisa Martínez Chacón, Luis Pedro Fernández, Gustavo Gabriel Voldman, Christopher J. Duffin, Juan Luis Alonso Alonso
Publikováno v:
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
A rock sample obtained from the Caliza Masiva of the San Emiliano Formation (Bashkirian–early Moscovian) in the Mina Profunda area (NE Villamanín) of the Bodón Nappe (Cantabrian Zone, NW Spain) has yielded numerous brachiopods and fish remains no
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::18d28058b631880639783088e2569969
http://hdl.handle.net/10651/56854
http://hdl.handle.net/10651/56854
Autor:
Sergey Oleynik, Oscar Merino-Tomé, Luis Pedro Fernández, Adam C. Maloof, Alison Campion, Javier Sanz-López, Blair Schoene, Juan R. Bahamonde, Silvia Blanco-Ferrera
Publikováno v:
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
MICYT, Ministerio de Ciencia y Tecnología; MINECO, Ministerio de Economía y Competitividad; Princeton, Princeton University; PEI, Princeton Environmental Institute, Princeton University; CGL2013-44458-P; CGL2016- 78738
Publikováno v:
Palaeogeography Palaeoclimatology Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 476 (2017) pp. 106-139
Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 476 (2017) pp. 106-139
The Valdorria carbonate platform, in northern Spain, features a well-preserved and continuous outcrop of a Bashkirian platform to basin transect. During the Asatauian (late Bashkirian), the platform growth changed gradually from a progradational to a
Publikováno v:
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
Lower-slope to basin-floor deposits associated to isolated microbial carbonate platforms of the Valdeteja Formation (Carboniferous foreland basin, Cantabrian Zone, NW Spain), containing large slid blocks and debrites, exhibit a combination of contrac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9639ece68a5313b275644b57540c100d
http://hdl.handle.net/10651/50584
http://hdl.handle.net/10651/50584
Autor:
Luis Pedro Fernández, Guillermo L. Albanesi, Aldo Lui Banchig, Gladys Ortega, Gustavo Gabriel Voldman, Raúl Cardó, Juan Luis Alonso Alonso
Publikováno v:
WOS:000449464900006
Andean geology v.45 n.3 2018
SciELO Chile
CONICYT Chile
instacron:CONICYT
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Andean geology v.45 n.3 2018
SciELO Chile
CONICYT Chile
instacron:CONICYT
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
The Rinconada Formation is a mélange that crops out in the eastern margin of the Argentine Precordillera, an exotic terrane accreted to Gondwana in Ordovician times. Its gravity-driven deposits have been studied by means of conodont and graptolite b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e0d0776cb3b703ef69f500028076ddb
http://hdl.handle.net/10651/50760
http://hdl.handle.net/10651/50760
Autor:
Paola Cianfarra, Matteo Maggi, A. Cuesta, Luis Pedro Fernández, Francesco Salvini, Simone Arragoni
The Central-Southern Apennines are the result of the collision between Europe and Africa. Despite the volume of existing literature, many problems remain unsolved such as the presence of Tertiary conglomerates containing exotic basement clasts. The l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::13bfe516527947b05233bd49b551b32a
http://hdl.handle.net/11567/988373
http://hdl.handle.net/11567/988373
Publikováno v:
Marine Geology. 356:71-87
Large-scale mass-transport deposits (MTDs) from two wedge-top depocentres in a Variscan foreland-basin system (Cantabrian Zone, Iberian Massif, northern Spain) have been studied to gain a better understanding of the processes involved in comparable d
Autor:
Angela Suárez, Alberto Marcos, Juan Luis Alonso Alonso, Luis Pedro Fernández, Elisa Villa, Oscar Merino-Tomé
Publikováno v:
International Geology Review. 57:563-580
Block-in-matrix formations in the Variscan foreland of Spain (Cantabrian Zone) occur in two different geological settings. The major block-in-matrix formations are melanges, which appear as carpets beneath or ahead of submarine thrust systems. These