1-20 OF 48 RESULTS FOR

Grigi Group

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 27–41.
... yielded 544 tridactyl footprints, arranged in 20 long trackways, and belongs to the upper part of the Calcari Grigi Group (lower portion of the Rotzo formation). All the tracks can be attributed to small-and medium-sized theropods. Trace fossils were discovered in a peritidal carbonate succession...
FIGURES | View All (9)
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...
FIGURES | View All (6)
Image
Stratigraphic column showing the lithological and paleontological compositi...
Published: 01 October 2011
FIGURE 2— Stratigraphic column showing the lithological and paleontological composition of the Calcari Grigi Group. In the right column a close view of the measured section with the track-bearing horizon.
Image
Hettangian–Sinemurian paleogeography. 1 = Lower Jurassic peritidal carbonat...
Published: 01 November 2012
Figure 9 Hettangian–Sinemurian paleogeography. 1 = Lower Jurassic peritidal carbonates named “Corna” in eastern Lombardy and the Monte Zugna Formation (Calcari Grigi Group) both in the Trento and Friuli platforms; 2 = deep-water deposits of the Belluno Basin (Soverzene Formation).
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2012
AAPG Bulletin (2012) 96 (11): 2065–2089.
...Figure 9 Hettangian–Sinemurian paleogeography. 1 = Lower Jurassic peritidal carbonates named “Corna” in eastern Lombardy and the Monte Zugna Formation (Calcari Grigi Group) both in the Trento and Friuli platforms; 2 = deep-water deposits of the Belluno Basin (Soverzene Formation). ...
FIGURES | View All (12)
Journal Article
Published: 01 October 2015
Journal of Foraminiferal Research (2015) 45 (4): 402–412.
..., 1972 ; Broglio Loriga & Neri, 1976 ; Septfontaine, 1984 , 1985 ; Bassoullet, 1997 ). The genus Lituosepta (type species Lituosepta recoarensis ) was first named by Cati (1959) for a lituolacean foraminifer discovered in the Calcari Grigi Group of the Southern Alps, northern Italy...
FIGURES | View All (5)
Journal Article
Published: 01 January 2006
Italian Journal of Geosciences (2006) 125 (1): 67–92.
... with epiclastic deposits, marked by a map-scale buried morphology of a caldera generation. The Valle dei Grigi-Fosso del Corbo and Laghi di Monticchio synthems are separated by an erosive contact marked by a palaeosol. In both cases, fault re-activation is documented. The Foggianello Synthem groups three...
Journal Article
Published: 01 June 2008
Italian Journal of Geosciences (2008) 127 (3): 389–405.
..., with the major early Toarcian transgressive peak being recorded in condensed facies with hardgrounds at Trnovski gozd, and marly limestone at Rumija. Regionally, the studied successions are correlative to formations of the western part of the Trento Plateau, i.e. to the Calcari Grigi Formation and the San...
Journal Article
Published: 01 April 2000
Journal of Foraminiferal Research (2000) 30 (2): 126–134.
... and Monte Grappa. The Calcari Grigi formation, whose thickness may reach more than 400–500 m in places, overlies the Dolomia Principale (Norian-Rhaetian), a succession of peritidal cycles ( Bosellini and Hardie, 1985 ). The Calcari Grigi are directly overlain by the Toarcian-Aalenian San Vigilio Group...
FIGURES | View All (7)
Journal Article
Published: 30 May 2016
Geological Magazine (2017) 154 (3): 625–650.
...; Schirolli, 1997 ; Meister, Schirolli & Dommergues, 2009 ); across much of the Trento Platform, the Hettangian–Sinemurian peritidal succession of the Calcari Grigi Group (Monte Zugna Formation) is unconformably overlain by a Sinemurian–Pliensbachian condensed succession...
FIGURES | View All (11)
Journal Article
Published: 01 January 2005
Italian Journal of Geosciences (2005) 124 (1): 301–312.
...Roberta Romano; Filippo Barattolo; Daniele Masetti; Anonymous Abstract The section studied is located at the eastern border of the Asiago plateaux close to the village of Foza. In this area, the Calcari Grigi are noticeably different from the classic succession subdivided into three members...
Journal Article
Journal: GSA Bulletin
Published: 06 February 2019
GSA Bulletin (2019) 131 (7-8): 1255–1275.
... systems at the Early Jurassic S–P Event and at the Late Triassic CPE. To this end, new carbonate and total organic carbon isotope (δ 13 C carb and δ 13 C TOC ) and biostratigraphic data from shallow (Calcari Grigi Group) and deep-water (Tofino Formation) successions deposited between the Hettangian...
FIGURES | View All (11)
Journal Article
Published: 01 October 2010
Italian Journal of Geosciences (2010) 129 (3): 457–495.
..., nella Carta geologica allegata, sono stati erroneamente associati al Gruppo della Scaglia ed contrassegnati con la sigla Mc. La formazione è costituita prevalentemente da marne nocciola e grigie che si alternano a calcilutiti e calcari marnosi grigi e nocciola con intercalati rari strati di arenarie...
Journal Article
Journal: PALAIOS
Published: 01 February 2004
PALAIOS (2004) 19 (1): 51–67.
... age. Northern Italian sites are located in the Calcari Grigi Formation on the South Trento carbonate platform, north of Verona in the Monte Lessini district ( Zempolich, 1993 ; Figs. 5B and 6 ; Appendix). The two Moroccan field sites are located in the Central and Eastern High Atlas Mountains...
FIGURES | View All (11)
Journal Article
Published: 01 February 2010
Italian Journal of Geosciences (2010) 129 (1): 74–90.
... of the Monticiano-Roccastrada Unit, which has been drilled down to 4900 m. The complex is composed of very low-grade metamorphic sequence belonging to two groups: ( a ) the Triassic Verrucano Group, composed of continental metapelites, metasandstones and metacon-glomerates; ( b ) the Palaeozoic Group, composed...
FIGURES | View All (13)
Journal Article
Published: 01 June 2009
Italian Journal of Geosciences (2009) 128 (2): 605–613.
..., hosting significant productive activities as well as important historical centers. Infrequent reverse-faulting earthquakes ( P ondrelli et alii , 2006 ) with M w up to 5.8 ( CPTI Working Group, 2004 ) pose a limited hazard but a comparatively high risk to most of these cities. In the decades...
FIGURES | View All (5)
Journal Article
Published: 01 July 2007
Journal of Foraminiferal Research (2007) 37 (3): 248–264.
FIGURES | View All (9)
Journal Article
Published: 01 April 2004
Journal of Foraminiferal Research (2004) 34 (2): 165–166.
... of their palaeoecology and taphonomy. . .” (from Abstract). F ugagnoli , A., Trophic regimes of benthic foraminiferal assemblages in Lower Jurassic shallow water carbonates from northeastern Italy (Calcari Grigi, Trento Platform, Venetian Prealps).—Palaeogeography, Palaeoclimatology, Palaeoecology, v. 205, no. 1–2...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1981
AAPG Bulletin (1981) 65 (3): 394–421.
... block ( Gaetani, 1975 ). On the Trento platform, peritidal limestones (Calcari Grigi) were widespread in the early Liassic, and during the middle Liassic a rim of oolite barrier bars protected a large lagoonal complex in which the huge pelecypod Lithiotis thrived and in which coaly deposits formed...
FIGURES | View All (28)
Journal Article
Published: 01 September 2011
Bulletin de la Société Géologique de France (2011) 182 (5): 405–415.
... al. , 2003 , 2005 ]. However, adult microconchs are quite common in some taxonomic groups ( Maceratites , Pelekodites and Otoites ). Most of these lower Bajocian ammonite shells represent ademic organisms and are interpreted as allochthonous elements arrived at their present location...
FIGURES | View All (11)