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Tremp Formation

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Journal Article
Published: 01 March 2016
Journal of Paleontology (2016) 90 (2): 250–268.
...Davinia Díez-Canseco; Luis A. Buatois; M. Gabriela Mángano; Margarita Díaz-Molina; M. Isabel Benito Abstract The Upper Cretaceous “redbeds” of the lower Tremp Formation (South-Central Pyrenees, Spain) contains an ichnofauna consisting of Taenidium barretti , Taenidium bowni , Loloichnus isp...
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Journal Article
Published: 01 September 1999
Bulletin de la Société Géologique de France (1999) 170 (5): 681–696.
...Nieves Lopez-Martinez; Pablo Pelaez-Campomanes Abstract Ten mammalian taxa have been recovered from four localities in the upper part of the Tremp Formation (south-central Pyrenees). Its stratigraphic position allows the localities to be correlated with the Sphaerochara edda charophyte zone...
Journal Article
Published: 01 January 1998
Bulletin de la Société Géologique de France (1998) 169 (1): 11–20.
...Nieves Lopez-Martinez; Luis Ardevol; Maria Eugenia Arribas; Jorge Civis; Angel Gonzalez-Delgado Abstract In the Ager basin and Benabarre area (southern Pyrenees, Spain), the Cretaceous-Tertiary (K/T) boundary is recorded in a succession of non-marine to coastal deposits (Lower Tremp Formation...
Journal Article
Published: 01 May 2016
Bulletin de la Société Géologique de France (2016) 187 (3): 133–153.
... the sequence stratigraphy interpretation. This formation is Early Eocene in age and crops out in several well-exposed cliffs in the Serraduy – Roda de Isabena area (Graus-Tremp basin, NE Spain). Within this succession, nineteen carbonate and siliciclastic facies have been identified and grouped...
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Image
Stratigraphic section of the Maastrichtian “redbeds” of the <b>Tremp</b> <b>Formation</b>...
Published: 01 March 2016
Figure 9 Stratigraphic section of the Maastrichtian “redbeds” of the Tremp Formation at Orcau locality, showing the vertical distribution of biogenic structures and other features: ( 1 ) mottling; ( 2 ) carbonate nodules; ( 3 ) paleosols; ( 4 ) root traces; ( 5 ) vertebrate tracks; ( 6
Journal Article
Published: 26 September 2016
Geological Magazine (2017) 154 (2): 393–398.
... skin impressions in the red-beds of the Tremp Formation (southern Pyrenees). The impressions are assigned to sauropods (probably titanosaurians) on the basis of their scale morphology, arrangement and size. They represent a valuable tool for analysing the last occurrences of the sauropod clade before...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2000
AAPG Bulletin (2000) 84 (4): 566–587.
... facies transitions (Vallcarga, Aren, and Tremp formations, respectively). The deltaic deposits are grouped into four depositional sequences based on recognition and definition of sequence boundaries and systems tracts. The basinward migration of the depocenters was associated with uplifting and cyclic...
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Summary model of ichnofaunal distribution in the fluvial-tidal transition o...
Published: 01 March 2016
Figure 11 Summary model of ichnofaunal distribution in the fluvial-tidal transition of the Tremp Formation. The mixed area and the fluvial-tidal channel are marked in terms of current dominance, whereas ichnology responds to salinity and is controlled by the salinity limit (modified from Buatois
Image
Figure  2 — Hainina pyrenaica  n. sp.  1,  FNT3-10 occlusal view of left P4...
Published: 01 July 2000
pairs; 7, FNT3-7, anterior view of left P2. All specimens from the Earliest Danian, Fontllonga-3, Tremp Formation (Lleida, Spain). Material stored in the Department of Paleontology, Complutense University of Madrid. Graphic scale represents 1 mm.
Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 267–280.
... part of the Tremp Formation, a short distance below the boundary with the overlying Figols Group in the Ilerdian stratotype area. The Ilerdian stage records a major marine transgression in the Pyrenees over the non-marine Tremp Formation ( Serra-Kiel et al. 1994 ). The existence of a major hiatus...
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Sedimentologic and paleontologic features in the “redbed” facies (Maastrich...
Published: 01 March 2016
Table 1 Sedimentologic and paleontologic features in the “redbed” facies (Maastrichtian Tremp Formation; modified from Díez-Canseco et al., 2014 ). Facies Lithologies Sedimentologic Features Body Fossils Other Features Depositional Environment Non-channelized deposits
Journal Article
Journal: Clay Minerals
Published: 01 March 2017
Clay Minerals (2017) 52 (1): 107–126.
... and biochronostratigraphic reconstruction of the Lower Tremp Formation (South-Central Pyrenees, Spain) around the Cretaceous/Palaeogene boundary . Sedimentary Geology , 312 , 31 – 49 . Domingo L. , López-Martínez N. , Soler-Gijón R. & Grimes S.T. ( 2007 ) A multi-proxy geochemical...
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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 1989
DOI: 10.2110/pec.89.44.0365
EISBN: 9781565761056
... Abstract Upper Cretaceous depositional-sequence architecture of the Tremp Basin in the Pyrenees reflects the effects of both subsidence and eustasy. Overall geometry is controlled by thermal subsidence, and depositional-sequence geometry, depositional facies, and sequence boundaries...
Journal Article
Published: 01 July 2000
Journal of Paleontology (2000) 74 (4): 701–711.
... pairs; 7, FNT3-7, anterior view of left P2. All specimens from the Earliest Danian, Fontllonga-3, Tremp Formation (Lleida, Spain). Material stored in the Department of Paleontology, Complutense University of Madrid. Graphic scale represents 1 mm. ...
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Journal Article
Journal: Geology
Published: 01 August 2003
Geology (2003) 31 (8): 689–692.
... intrabasinal relationships among weathering, soil formation, and transport of debris to the sea during the initial Eocene thermal maximum. The deposits discussed here are in the Basque basin in the southeastern Pyrenees and the Tremp basin in the south-central Pyrenees ( Schmitz et al., 2001 ). Bathyal...
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Journal Article
Journal: Clay Minerals
Published: 01 March 2011
Clay Minerals (2011) 46 (1): 105–126.
... Formation, or Tremp Group (e.g. Eichenseer, 1988 ; Cuevas, 1992 ; López-Martínez & Peláez-Campomanes, 1999 ; Rosell et al. , 2001 ). The Tremp Group is subdivided into two main parts. The lower one, dominantly siliciclastic, is clearly Cretaceous in age, as demonstrated by abundant dinosaur...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 2008
AAPG Bulletin (2008) 92 (2): 249–269.
... and Tremp formations (e.g., Nagtegaal et al., 1983 ; Simó and Puigdefàbregas, 1985 ; Simó, 1986 , 1989 ; Díaz-Molina, 1987 ; Mutti and Sgavetti, 1987 ; Sgavetti, 1992 , 1994 ; Ardèvol et al., 1993 , 2000 ; Déramond et al., 1993 ; Rosell, 1994 ; Arbués et al., 1996 ). For this, we used...
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General stratigraphy (names of <b>formations</b> are informal), main lithologies a...
Published: 01 May 2016
Fig. 2 General stratigraphy (names of formations are informal), main lithologies and depositional environments of the Early Eocene series of the Graus-Tremp basin. Paleogene zonations of larger foraminifera [ Gradstein et al. , 2004 ; Serra-Kiel et al. , 1994 ].
Journal Article
Journal: PALAIOS
Published: 01 August 2001
PALAIOS (2001) 16 (4): 409–416.
... thrust units constituting the southern part of the Pyrenean Range ( Puigdefabregas et al., 1986 ). The coastal and continental deposits of the Cretaceous-Tertiary transition reach nearly 1000 m in thickness and consist of two stratigraphic units: the Arén Formation and the Tremp Group (also known...
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Journal Article
Journal: Geology
Published: 01 March 2007
Geology (2007) 35 (3): 215–218.
... stage of conglomerate formation. In the study area, the Tremp-Graus basin ( Fig. 1 ; GSA Data Repository Fig. DR1 1 ), latest Cretaceous and early Paleogene continental deposits, the “Garumnian” facies, are well preserved and can be studied in a number of exposures in a transect over ∼80 km...
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