Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Margarita Díaz-Molina"'
Autor:
Xavier Delclòs Martínez, Margarita Díaz Molina, María de los Angeles Bustillo Revuelta, Pablo Peláez-Campomanes de Labra, Borja Sanchiz, Enrique Peñalver Mollá, María José López García, Rosario Rodríguez Talavera
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Digital.CSIC. Repositorio Institucional del CSIC
instname
Universidad de Barcelona
Digital.CSIC. Repositorio Institucional del CSIC
instname
[EN] Purpose: A new Iberian Konservat-Lagerstätte discovered in Tresjuncos (Cuenca, Spain) is described and interpreted based on geological and paleontological information. Methods: The samples were studied using conventional mineralogical (powder X
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db47fca5068eb933a1965ac24d29b9a2
http://hdl.handle.net/2445/163339
http://hdl.handle.net/2445/163339
Autor:
Margarita Díaz-Molina, Davinia Díez-Canseco, Ignacio Arenillas, José A. Arz, Mª Isabel Benito
Publikováno v:
Sedimentary Geology. 312:31-49
The Upper Cretaceous–Paleogene deposits of the Grey Unit, the Lower Red Unit and the Suterranya Limestone of the Tremp Formation (South-Central Pyrenees) preserve sedimentological and palaeontological features that suggest a connection with marine
Autor:
Davinia Díez-Canseco, Margarita Díaz-Molina, M. Isabel Benito, M. Gabriela Mángano, Luis A. Buatois
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
The Upper Cretaceous “redbeds” of the lower Tremp Formation (South-Central Pyrenees, Spain) contains an ichnofauna consisting of Taenidium barretti, Taenidium bowni, Loloichnus isp., Arenicolites isp., Planolites isp., and Palaeophycus isp. This
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b881af000a56f419fab1cc626736759
http://hdl.handle.net/10261/184645
http://hdl.handle.net/10261/184645
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
The Late Cretaceous Aren Fm exposed north of Bastus in the Tremp Basin (south-central Pyrenees) preserves an excellent record of dinosaur eggs laid in a marine littoral setting. Different from other cases reported in literature, at the Bastus site th
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
ResearcherID
Spanish Journal of Palaeontology, Vol 27, Iss 2, Pp 93-104 (2020)
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
ResearcherID
Spanish Journal of Palaeontology, Vol 27, Iss 2, Pp 93-104 (2020)
The Middle Miocene sediments exposed in Somosaguas contain an excellent record of mammal fossil remains preserved in debris and mudfl ow deposits. In the sedimentary sequence of Somosaguas three facies associations are distinguished, representing all
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5efa513a7e28fc2db6e163f799e2b68b
Autor:
O. Kälin, Nieves López-Martínez, José J. Moratalla, Monique Vianey-Liaud, Margarita Díaz-Molina, José Luis Sanz
Publikováno v:
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
Publikováno v:
Estudios Geológicos. 43
In this work we aim to resconstruct the paleoenvironmental context of the Galve archosaurs. The archosaurs remains are most frequently found in the lower 500 m of the Early Cretaceous succession. This succession is subdivided into four units which ov
Autor:
Margarita Díaz Molina
Publikováno v:
Estudios Geológicos. 43
The Tremp Formation is the continental lateral equivalent of the Aren Sandstone Formation. Both formations are part of regressive depositional sequences, formed during a relative sea level rise. At the top of the Isona anticline and in tbe south flan