Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Alfonso Yébenes"'
Publikováno v:
Spanish Journal of Palaeontology, Vol 24, Iss 1, Pp 47-58 (2021)
El yacimiento de Torrellano (Mioceno Superior, provincia de Alicante) ha proporcionado cientos de fragmentos de cáscara de tipo básico ornitoide, caracterizadas fundamentalmente por su gran grosor y por presentar los poros en el interior de hendidu
Publikováno v:
Geo-Marine Letters. 40:341-361
This research explores the Messinian record in a western Mediterranean basin at the eastern end of the Betic Cordillera (the Garruchal section, southern sector of the Bajo Segura basin). Sedimentary facies development and foraminiferal assemblages we
Autor:
Jaume Dinarès-Turell, Carlos Lancis, Antonio Estévez, Hugo Corbí, José-Enrique Tent-Manclús, Jesús-Esteban Caracuel, J. M. Soria, Alfonso Yébenes
Publikováno v:
Geobios. 43:201-217
The Fortuna Basin is an example of a marginal Mediterranean basin with evaporitic sedimentation during the Late Tortonian and Messinian. This basin shows an early restriction event before the main Messinian Salinity Crisis (MSC) that allows the Torto
Autor:
Jesús M. Soria, Antonio Estévez, Jaume Dinarès-Turell, Alfonso Yébenes, Carlos Lancis, Jesús E. Caracuel, Jose Enrique Tent-Manclus
Publikováno v:
Comptes Rendus Geoscience. 340:474-481
The Neogene Fortuna and Bajo Segura basins are located on the northeastern end of the Trans-Alboran Shear Zone (TASZ), on the eastern Betic cordillera. The stratigraphic study of the infilling of these basins has shown two major sedimentary discontin
Autor:
Carlos Lancis, Jesús E. Caracuel, Jesús M. Soria, Alfonso Yébenes, Jaume Dinarès-Turell, Jose Enrique Tent-Manclus, Hugo Corbí, César Viseras
Publikováno v:
Sedimentary Geology. 203:267-288
The analysis of the Messinian and Pliocene stratigraphy of the southern Bajo Segura Basin (Betic Cordillera, Spain) has revealed three highstand sedimentary phases (Messinian I, Messinian II, and Pliocene) bounded by two lowstand erosional surfaces (
Publikováno v:
Sedimentary Geology. 179:225-247
The Bajo Segura Basin is a marginal basin of the Western Mediterranean located on the eastern end of the Betic Cordillera (southeastern Spain). Its Messinian and Pliocene stratigraphic record is divided into four allostratigraphic units, with boundin
Publikováno v:
Sedimentary Geology. 169:121-128
The Messinian salinity crisis is recorded on the northern margin of the Bajo Segura Basin by lacustrine and fluvial deposits coeval to the evaporites that precipitated in the basin’s central areas. These syn-evaporitic Messinian deposits are bounde
Publikováno v:
Geomorphology. 42:197-211
The Serra Gelada sea cliffs are carved in Mesozoic carbonate rocks belonging to the External Zones of the eastern Betic Cordillera (Alicante, SE Spain). Several normal faults with vertical slips of more than a hundred metres have played an important
Autor:
Jesús E. Caracuel, Alice Giannetti, J. M. Soria, Alfonso Yébenes, Jose Enrique Tent-Manclus, Paolo Monaco, Hugo Corbí
A detailed sedimentological and paleontological analysis of the uppermost Miocene (Messinian)–Pliocene boundary at the northern border of the Bajo Segura Basin, southeastern Spain, was carried out in order to describe the evolution of the regional
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bd440f6c64f700287a1d4b4873ebb4c0
http://hdl.handle.net/11391/714527
http://hdl.handle.net/11391/714527
Autor:
José Luis Goy, Alfonso Yébenes, Ángel F. González, Cristino J. Dabrio, Claude Hillaire-Marcel, Michel Preda, Teresa Bardají, Jorge Civis, Cari Zazo, Bassam Ghaleb, Alessandro M. Forte
Publikováno v:
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Digital.CSIC. Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Digital.CSIC. Repositorio Institucional del CSIC
The elevation and timing of high sea stands during Oxygen Isotope Stage (OIS) 7 are not as well constrained as those of OIS 5e. Conflicting values are reported from Mediterranean coastlines, and fossil dating is inaccurate because of ubiquitous open
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b6c48c40277e581b47c6f4d24a18a5e