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Rotzo Formation

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Stratigraphic section of the <b>Rotzo</b> <b>formation</b> at the Coste dell’Anglone dino...
Published: 01 February 2011
Fig. 4 Stratigraphic section of the Rotzo formation at the Coste dell’Anglone dinosaur tracksite. The track-bearing horizon is in the top surface of the second shallowing upward cycle.
Journal Article
Journal: PALAIOS
Published: 01 October 2011
PALAIOS (2011) 26 (10): 601–606.
... 1918, presumably to connect the front- with the back line. The tracks are tridactyl, two of which are organized in a trackway, and provide evidence for the presence of medium-sized theropods. The track-bearing horizon is situated at the base of the Rotzo formation (Calcari Grigi Group), within shallow...
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Image
Microfacies of platform carbonates from Viote and Santa Massenza sections i...
Published: 06 February 2019
. Lower Rotzo Formation, meter 28.95 of the Viote section. (C) Foraminiferal floatstone with crinoids (cr). Foraminifers are mostly Orbitopsella (orb). Fully micritized foraminifers (e.g., m-orb) may resemble micritic intraclasts or peloids. Detail in F. Rotzo Formation, meter 33.90 of the Viote section
Journal Article
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 27–41.
...Fig. 4 Stratigraphic section of the Rotzo formation at the Coste dell’Anglone dinosaur tracksite. The track-bearing horizon is in the top surface of the second shallowing upward cycle. ...
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Image
Pliensbachian paleogeography. 1 = Pliensbachian platform carbonates (<b>Rotzo</b> ...
Published: 01 November 2012
Figure 10 Pliensbachian paleogeography. 1 = Pliensbachian platform carbonates (Rotzo Formation in the Trento platform); 2 = marginal calcarenitic bodies (Massone Oolite in the Trento platform and in the Po Plain); 3 = condensed deposits (Fanes Piccola Encrinite in the Trento and Friuli plateaus
Image
Comparison between surface and subsurface type-successions inside the diffe...
Published: 01 November 2012
Figure 8 Comparison between surface and subsurface type-successions inside the different tectonostratigraphic domains of the southern Alps. Note the different scale. DP = Dolomia Principale; ZG = Monte Zugna Formation; OL = Loppio Oolitic Limestone; RZ = Rotzo Formation; CG = undifferentiated
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Chemostratigraphic transect across different types of Jurassic successions ...
Published: 30 May 2016
Formation; OL – Loppio Oolitic Limestone; RZ – Rotzo Formation; CG – undifferentiated Calcari Grigi; OM – Massone Oolite; ENF – Fanes Piccola Encrinite; OSV – San Vigilio Oolite + Tenno Formation; SOV – Soverzene Formation; IGNE – Igne Formation; ARV – Rosso
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2012
AAPG Bulletin (2012) 96 (11): 2065–2089.
...Figure 10 Pliensbachian paleogeography. 1 = Pliensbachian platform carbonates (Rotzo Formation in the Trento platform); 2 = marginal calcarenitic bodies (Massone Oolite in the Trento platform and in the Po Plain); 3 = condensed deposits (Fanes Piccola Encrinite in the Trento and Friuli plateaus...
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Image
Comparison of changes in carbonate factory and platform geometry across S–P...
Published: 06 February 2019
formations to overlying Rotzo Formation on the Trento Platform at Monte Roite (45°48′31.57″N, 11°9′40.10″E). (B) Late Triassic: contact between Cassian Dolomite carbonate platform and overlying Heiligkreuz Formation at Lagazuoi (46°31′38.11″N, 12°1′20.18″E). Fm.—Formation; LOP—Loppio; S–P—Sinemurian
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Distribution of different types of Jurassic successions inside the main pal...
Published: 01 November 2012
Formation; OL = Loppio Oolitic Limestone; RZ = Rotzo Formation; CG = undifferentiated Calcari Grigi; OM = Massone Oolite; ENF = Fanes Piccola Encrinite; OSV = San Vigilio Oolite + Tenno Formation; SOV = Soverzene Formation; IGNE = Igne Formation; RAV = Rosso Ammonitico Veronese; VJ = Vajont Limestone; CEL
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Previously published ( Franceschi et al., 2014a ) bulk-carbonate δ 13 C car...
Published: 06 February 2019
Figure 6. Previously published ( Franceschi et al., 2014a ) bulk-carbonate δ 13 C carb record for Monte Zugna, Loppio, and Rotzo formations straddling the Sinemurian/Pliensbachian boundary in Viote section atop the Trento Platform in Italy. Note unconformity associated with S–P Event in δ 13 C
Journal Article
Published: 01 January 2005
Italian Journal of Geosciences (2005) 124 (1): 301–312.
... Mesozoic micrite microfossils Middle Oolitic Member oolite Plantae Prealps Protista Rotzo Formation San Vigilio Group sedimentary rocks sediments Sinemurian Southern Europe stratigraphic gaps subtidal environment Trento Platform Triassic unconformities Upper Triassic Veneto Italy ...
Journal Article
Journal: GSA Bulletin
Published: 06 February 2019
GSA Bulletin (2019) 131 (7-8): 1255–1275.
.... Lower Rotzo Formation, meter 28.95 of the Viote section. (C) Foraminiferal floatstone with crinoids (cr). Foraminifers are mostly Orbitopsella (orb). Fully micritized foraminifers (e.g., m-orb) may resemble micritic intraclasts or peloids. Detail in F. Rotzo Formation, meter 33.90 of the Viote section...
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Journal Article
Published: 30 May 2016
Geological Magazine (2017) 154 (3): 625–650.
... Formation; OL – Loppio Oolitic Limestone; RZ – Rotzo Formation; CG – undifferentiated Calcari Grigi; OM – Massone Oolite; ENF – Fanes Piccola Encrinite; OSV – San Vigilio Oolite + Tenno Formation; SOV – Soverzene Formation; IGNE – Igne Formation; ARV – Rosso...
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Image
Schematic stratigraphic setting of the Formazione di <b>Rotzo</b> in the Tonezza d...
Published: 01 October 2015
Fig. 2.— Schematic stratigraphic setting of the Formazione di Rotzo in the Tonezza del Cimone area (Trento Platform, Early Jurassic) and the section studied. The bivalve carpet succession (∼ 7 m-thick) is located in the upper part of the formation, within the Lituosepta compressa Zone, about 25
Journal Article
Published: 01 April 2000
Journal of Foraminiferal Research (2000) 30 (2): 126–134.
... the Liassic Rotzo Member (Calcari Grigi formation, Venetian Prealps), provides us new biostratigraphic data about the genus Everticyclammina Redmond 1964 . A new species of Everticyclammina, E. praevirguliana n. sp., is formally described from the Calcari Grigi, where it occurs in levels attributed...
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Journal Article
Journal: PALAIOS
Published: 01 October 2015
PALAIOS (2015) 30 (10): 758–770.
...Fig. 2.— Schematic stratigraphic setting of the Formazione di Rotzo in the Tonezza del Cimone area (Trento Platform, Early Jurassic) and the section studied. The bivalve carpet succession (∼ 7 m-thick) is located in the upper part of the formation, within the Lituosepta compressa Zone, about 25...
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Journal Article
Published: 01 October 2015
Journal of Foraminiferal Research (2015) 45 (4): 402–412.
...) and the Formazione di Rotzo ( ca . 35 m thick), both belonging to the Calcari Grigi Group (Hettangian–Pliensbachian), up to the stratigraphic contact with the overlying Rosso Ammonitico Veronese Formation (Aalenian–Tithonian; Martire et al., 2006 ). The lower part of the section consists mainly of poorly...
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Journal Article
Published: 01 April 2004
Journal of Foraminiferal Research (2004) 34 (2): 165–166.
..., 2004, p. 111–130, 6 figures, 4 plates.—“Benthic foraminiferal distribution patterns in the Lower Jurassic Rotzo Member (Trento Platform, northeastern Italy) are analysed in terms of trophic gradients to provide a better understanding of the benthic communities during the time of the initial...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP290.13
EISBN: 9781862395381
... incompetent unit including the Rotzo, St Vigilio oolitic limestone, Ammonitico Rosso and Maiolica formations (Fig. 2 ). The poly-deformed Gamonda–Tormeno relay zone records two different tectonic regimes (Fig. 11 ). Prolonged extensional activity started in the Lias and ended in the Palaeogene, followed...
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