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Marne a Fucoidi Formation

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Journal Article
Journal: Palynology
Published: 01 July 2016
Palynology (2016) 40 (2): 230-246.
... Formation (Tithonian–lowermost Aptian) and the polychrome marls of the Marne a Fucoidi Formation (Aptian–Albian). The Oceanic Anoxic Event 1a (OAE 1a) anoxic horizon (Selli Level) is located in the latter formation. Here, we report for the first time a palynostratigraphical assessment of this key section...
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... Soft-sediment deformation structures crop out in the Lower Cretaceous succession of the Gubbio anticline in the Umbria-Marche Apennines of Italy. The deformation interval is ~13 m thick and occurs between the upper Hauterivian–lower Aptian Maiolica Formation and the Aptian Marne a Fucoidi...
Journal Article
Published: 01 January 1974
Italian Journal of Geosciences (1974) 93 (3): 567-573.
...G. Deiana; U. Pieruccini GeoRef, Copyright 2012, American Geosciences Institute. 1974 Apennines Coniferales Europe fossil wood Gymnospermae Italy lithostratigraphy Marches Italy Marne a Fucoidi Formation Mesozoic Montelago Plain occurrence paleobotany Plantae Southern Europe...
Journal Article
Published: 01 October 2019
Italian Journal of Geosciences (2019) 138 (3): 333-354.
...) Jurassic condensed succession (Bugarone Group); E) Lower Cretaceous pelagites (Maiolica and Marne a Fucoidi formations); F) Upper Cretaceous-Palaeogene p.p. carbonates (Scaglia Bianca, Scaglia Rossa and Scaglia Variegata formations); G) Palaeogene p.p .-Neogene deposits (Scaglia Cinerea, Bisciaro...
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Series: GSA Special Papers
Published: 11 September 2019
DOI: 10.1130/2019.2542(12)
EISBN: 9780813795423
... the fragments apart. The breccia is bounded stratigraphically above by the middle Cretaceous Marne a Fucoidi (Fucoid marls), which appears to represent an aquiclude that limited the volume of high fluid pressure ( P F ). Although the mechanism of formation of the expansion breccias is not yet clear, we list...
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Journal Article
Published: 01 January 2000
Italian Journal of Geosciences (2000) 119 (3): 655-665.
... Institute. 2000 Apennines Bianca Formation Bisciaro Formation Cenozoic Central Apennines deformation Diasprigni Limestone Europe extension tectonics faults folds Italy Marches Italy Marne a Fucoidi Formation Mesozoic Miocene models Mount Galenne Mount Galloro Neogene Perugia Italy...
Journal Article
Published: 01 June 2019
Italian Journal of Geosciences (2019) 138 (2): 274-295.
... and alluvium deposits (Holocene-Pleistocene); 2. Marnoso Arenacea (middle Miocene); 3. Schlier (middle Miocene); 4. Bisciaro (lower Miocene); 5. Scaglia Cinerea (lower Miocene-upper Eocene); 6. Scaglia Rossa and Variegata (lower Eocene-upper Cretaceous); 7. Scaglia Bianca (lower Cretaceous); 8. Marne a Fucoidi...
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.... Menichetti that focuses on the soft-sediment deformation structures observed in the lower Cretaceous successions along the Gubbio anticline between the Maiolica and the Marne a Fucoidi Formations. These slump structures suggest the existence of a local paleoslope dipping toward the north-northwest, where...
FIGURES
Journal Article
Published: 01 June 2009
Italian Journal of Geosciences (2009) 128 (2): 341-352.
.... They are characterized by the F5-F8-F9a and F8-F9a facies associations. Several silicified siltitic-marly turbidite layers with black cherty centimetre-scale bands and nodules are present in the basal portion of this formation («cherty lithofacies-REN a »). It corresponds to the «Marne silicee di Monte Sperello» of B...
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Journal Article
Published: 01 February 2017
Italian Journal of Geosciences (2017) 136 (1): 125-135.
... sides of the Salinello Valley, apart from the Salinello Gorge, where the east-dipping right-way-up Montagna dei Fiori monocline overthrusts the west-dipping overturned to recumbent outer sector of the forelimb, which exposes the Marne a Fucoidi and Scaglia formations ( Fig. 5 , Table. 1). The Marne...
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Series: GSA Special Papers
Published: 11 September 2019
DOI: 10.1130/2019.2542(11)
EISBN: 9780813795423
... and synsedimentary faulting within the upper part of the Maiolica Formation and the lower part of the overlying Marne a Fucoidi Formation ( Menichetti, 2016 ). After that, the Umbria-Marche pelagic basin experienced a long period of tectonic quiescence. Synsedimentary extensional tectonism resumed in the Lower...
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Journal Article
Published: 01 October 2015
Italian Journal of Geosciences (2015) 134 (3): 556-575.
... , which attains a thickness of 400–500 m ( P avan & P irini , 1966) . According to the same authors, the overlaying Marne a Fucoidi and Scaglia formations ( fig. 2B ) are collectively ~400 m thick; in addition, the uppermost part of the former Scaglia and probable Eocene carbonates, both...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2016
GSA Bulletin (2016) 128 (11-12): 1660-1678.
... the Marne a Fucoidi Formation ( Fig. 3B ). The landslide in between these two is the great landslide of Portonovo, which is remarkably similar, in terms of geometry and size, to the huge and more famous Marcus landslide ( Fig. 4 ), a Pleistocene structure located in the McDowell Mountains Park in Arizona...
Journal Article
Published: 01 June 2017
Italian Journal of Geosciences (2017) 136 (2): 186-197.
... the Maiolica Fm. The main aquifer in the studied area is represented by the Scaglia Fm., already exploited for water supply with two deep wells (n. 1 and 2 in Fig. 1 ), at a depth of 280 m. The Scaglia aquifer is confined by two impervious marly formations: the Cretaceous Marne a Fucoidi Fm...
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Series: GSA Special Papers
Published: 11 September 2019
DOI: 10.1130/2019.2542(13)
EISBN: 9780813795423
... ABSTRACT The geochemical signatures of sparry calcite-sealing expansion breccias, calcite veins, and host clasts were analyzed for their strontium ( 87 Sr/ 86 Sr) and oxygen and carbon (δ 18 O, δ 13 C) stable isotopic signatures. The breccias occur within the Lower Cretaceous Maiolica Formation...
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Journal Article
Published: 01 October 2015
Italian Journal of Geosciences (2015) 134 (3): 495-512.
... . The formations of the Umbria-Marche stratigraphic sequence exposed in the Conero are the Maiolica Fm., the Marne a Fucoidi Fm., and the Scaglia Rossa Fm. ( fig. 1 ; B ortolotti et alii , 1994 ; M ontanari & S androni , 1995) . The stratigraphic sequence of the Monte Conero has some...
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Journal Article
Published: 01 June 2009
Bulletin of the Seismological Society of America (2009) 99 (3): 1612-1635.
... of the Scaglia Bianca Formation (lower Cretaceous–middle Cretaceous), (6) marls of the Marne a Fucoidi Formation (lower Cretaceous), (7) alluvial fan, (8) borehole location, (9) attitude of beds, (10) supposed fault, (11) certain fault, and (12) anticline axis. The geological substratum of the valley...
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Series: GSA Special Papers
Published: 11 September 2019
DOI: 10.1130/2019.2542(01)
EISBN: 9780813795423
...–Albian Marne a Fucoidi (Fucoid marls) up until about the end of the Oligocene, the facies and thicknesses of the formations are comparable across the depositional basin, with only a few distinctive differences, for example, the presence of white calcareous turbidites in the Scaglia rossa...
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Journal Article
Published: 01 February 2018
Italian Journal of Geosciences (2018) 137 (1): 62-72.
...), Marne a Fucoidi (albian-Aptian), Scaglia Bianca and Scaglia Rossa formations (Upper Cretaceous-Eocene). The Calcare Massiccio Formation is made up of massive limestones, characterised by intense fracturing and karst phenomena. The Bugarone Formation (Aalenian-Tithonian) is constituted...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1991
AAPG Bulletin (1991) 75 (4): 832-844.
... occurred in the Jurassic, leading to normal faulting and rapid subsidence on the Apulian margin. More pelagic facies (Maiolica) progressively appeared and persisted through the Cretaceous. The middle Cretaceous (Albian-Cenoma-nian) anoxic event led to the deposition of organic-rich marls (Marne a Fucoidi...
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