Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Mariano Marzo"'
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
The Hawaz Formation comprises a siliciclastic, shallow to transitional marginal marine succession, deposited on the north-western cratonic margin of Gondwana during the Middle Ordovician. This unit is well documented in the north central part of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cddaa9cf62d595e17beed67c8778775e
http://hdl.handle.net/2445/184658
http://hdl.handle.net/2445/184658
Autor:
Carpio, Mariano Marzo
Publikováno v:
Ayer, 2007 Jan 01(65), 45-68.
Externí odkaz:
https://www.jstor.org/stable/41325070
Autor:
Carpio, Mariano Marzo
Publikováno v:
Mientras Tanto, 2006 Apr 01(98), 105-121.
Externí odkaz:
https://www.jstor.org/stable/27821165
Autor:
Patricia Cabello, M. López-Blanco, María H. Murillo-López, David García-Sellés, David Domínguez, Jose Luis Cuevas, Mariano Marzo, Pau Arbués
Publikováno v:
Marine and Petroleum Geology. 94:19-42
The Pont de Montanyana outcrop exposes strata of the lower Eocene Montllobat Formation deposited in alluvial plains and in meandering river systems of the Tremp-Graus piggyback basin (Southern Pyrenees, Spain). This article focuses on the characteris
Autor:
Mariano Marzo, F. J. Luque, Jacinto Alonso-Azcárate, Ausonio Ronchi, Raúl de la Horra, José López-Gómez, Violeta Borruel-Abadía, Ana Belén Galán-Abellán, José F. Barrenechea
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
In recent years there is growing evidence of the importance of the Smithian-Spathian (Early Triassic) ecological crisis to explain the delayed recovery of life after the Permian-Triassic Boundary mass extinction. This study focuses on sedimentary con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d80963e14c695d2abd98966bc9341c5
http://hdl.handle.net/10261/187358
http://hdl.handle.net/10261/187358
Autor:
José María Tubía, Jacinto Alonso-Azcárate, Ana Márquez-Aliaga, David Gómez-Gras, Javier Luque, Emilio Ramos, Henar Vargas, Sylvie Bourquin, Alfonso Sopeña, Mariano Marzo, Alfredo Arche, Y. Sánchez-Moya, Carlos Galé, Juan Alberto Pérez-Valera, Lidia Rodríguez-Méndez, Belén Galán-Abellán, Alberto Pérez-López, Ramon Mercedes-Martín, Nicola Gretter, Julia Cuevas, Ángela Suárez-Rodríguez, Pablo Plasencia, Fidel Martín-González, Javier Martín-Chivelet, Agustín Martín-Algarra, María José Escudero-Mozo, Fernando Pérez-Valera, Leopoldo Márquez, Blas Lorenzo Valero Garcés, Nemesio Heredia Carballo, Teresa Ubide, Ausonio Ronchi, Marceliano Lago, José F. Barrenechea, Raúl de la Horra, César Viseras, Patricia Cadenas, José Gisbert Aguilar, Ramon Salas, Antonio Goy, José B. Diez, David Sánchez-Fernández, José Arribas, Gabriela Fernández-Viejo, José López-Gómez, Federico Ortí, Violeta Borruel-Abadía, Jorge M. Gaspar-Escribano, Joan Lloret
Publikováno v:
The Geology of Iberia: A Geodynamic Approach. Volume 3: The Alpine Cycle
Cecilio Quesada; José Tomás Oliveira. The Geology of Iberia: A Geodynamic Approach. Volume 3: The Alpine Cycle, pp.29-112, 2019, Regional Geology Reviews book series, 9783030112943
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030112943
HAL
Digital.CSIC. Repositorio Institucional del CSIC
instname
Cecilio Quesada; José Tomás Oliveira. The Geology of Iberia: A Geodynamic Approach. Volume 3: The Alpine Cycle, pp.29-112, 2019, Regional Geology Reviews book series, 9783030112943
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030112943
HAL
Digital.CSIC. Repositorio Institucional del CSIC
instname
International audience; The Permian-Triassic rifting represents the first of the two Mesozoic rifting stages recorded in the Iberian Peninsula. Its first phases of development started during the Early Permian, and were linked to the beginning of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b9b2181c04978a75cff5018252b63a87
https://hal-insu.archives-ouvertes.fr/insu-02169277
https://hal-insu.archives-ouvertes.fr/insu-02169277
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
The subsurface of the highly productive Murzuq Basin in southwest Libya remains poorly understood. As a consequence, a need exists for detailed sedimentological studies of both the oil-prone Mamuniyat Formation and Hawaz Formation reservoirs in this
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bd94460fdce220dcd07b0fc813f5453b
http://hdl.handle.net/2445/161896
http://hdl.handle.net/2445/161896
Autor:
Raúl de la Horra, Alfredo Arche, José F. Barrenechea, Belén Galán-Abellán, Mariano Marzo, José López-Gómez
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
instname
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The Early–Middle Triassic siliciclastic deposits of the Catalan Ranges, NE Spain, are dominated by aeolian sediments indicating a predominance of arid climate during this time span, in sharp contrast with the coeval fluvial sediments found in the C
Autor:
Marc Durand, Raúl de la Horra, Belén Galán-Abellán, José F. Barrenechea, Alfredo Arche, José López-Gómez, Sylvie Bourquin, Mariano Marzo
Publikováno v:
Sedimentary Geology
Sedimentary Geology, Elsevier, 2012, 249-250, pp.26-44
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Sedimentary Geology, 2012, 249-250, pp.26-44. ⟨10.1016/j.sedgeo.2012.01.006⟩
Sedimentary Geology, Elsevier, 2012, 249-250, pp.26-44
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Sedimentary Geology, 2012, 249-250, pp.26-44. ⟨10.1016/j.sedgeo.2012.01.006⟩
The Permian–Triassic transition (P–T) was marked by important geochemical perturbations and the largest known life crisis. Consequences of this event, as oxygen-depleted conditions and the unusual behavior of the carbon cycle, were prolonged duri
Trace fossils and depositional environments in the Hawaz Formation, Middle Ordovician, western Libya
Publikováno v:
Journal of African Earth Sciences. 60:28-37
The ichnology of the Middle Ordovician Hawaz Formation in the Gargaf uplift (W Libya) is here reported. Eleven ichnogenera have been identified in this shallow marine formation: Arthrophycus , Bergaueria , Cruziana , Daedalus , Lockeia , cf. Psammich