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Calcari a Briozoi e Litotamni Formation

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Journal Article
Published: 01 January 2002
Italian Journal of Geosciences (2002) 121 (2): 179–186.
...Marco Brandano Abstract This paper describes a rhodolitic level in the Lower-Middle Miocene succession ("Calcari a Briozoi e Litotamni" Formation) outcropping near the village of Tagliacozzo (Carseolani Mts., Central Apennines). The "Calcari a Briozoi e Litotamni" Formation represents the Cenozoic...
Journal Article
Published: 01 October 2012
Italian Journal of Geosciences (2012) 131 (3): 359–372.
... to the Cretacic “ Calcari a Rudiste e Orbitoline ” Formation and to the Miocene “ Calcari a Briozoi e LitotamniFormation ( Foglio CARG, 2009 ) – and related to the Cicolano-Western Marsica Unit of P ierantoni et alii (this issue) – outcrop rather continuously, displaying a general sub-horizontal-to-low...
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Journal Article
Journal: Geology
Published: 01 June 2011
Geology (2011) 39 (6): 527–530.
... Campetello is interpreted as a sackung-type slope deformation, where the movement (toward the northeast) is possibly accommodated along the downslope-dipping stratigraphic limit between the Calcari a Briozoi e Litotamni Formation and the Calcari Spongoliti Unit ( Fig. 3A ). The maximum D LoS of ∼4.5 cm...
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Journal Article
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 75–92.
... in sedimentary carbonates . AAPG Bull. , 54 , 207 – 244 . Civitelli G. Brandano M. ( 2005 ) - Atlante delle litofacies e modello deposizionale dei Calcari a Briozoi e Litotamni nella Piattaforma carbonatica laziale-abbruzzese . Boll. Soc. Geol. It. , 124 , 611 – 643 . Coates D.F...
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Journal Article
Published: 01 July 2012
Journal of Sedimentary Research (2012) 82 (7): 451–463.
... e-mail: marco.brandano@uniroma1.it SEPM (Society for Sedimentary Geology) 2012 Seagrasses have two clearly distinguishable levels: the rhizomes and the blades. Each level has characteristic associated communities that live attached to the plant ( Langer 1988 ; Mateu-Vicens et al. 2010...
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Journal Article
Published: 01 October 2011
Italian Journal of Geosciences (2011) 130 (3): 352–369.
... Linaro). This structure consists of Meso-Cenozoic and Plio-Pleistocene sedimentary units and Pleistocene volcanic deposits. The Meso-Cenozoic sequence belongs to the allochtonous flyschs known as “Serie dei flysch tolfetani e della Pietraforte” or Tolfa Formation, which are Cretaceous to Oligocene in age...
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Image
A: Three-dimensional view and geological cross section for Colle Campetello...
in > Geology
Published: 01 June 2011
a Nummuliti e Discocycline (Early Paleocene); 3—Calcari a Miogypsine e Lepidocycline (Early-Middle Paleocene); 4—Calcari Spongoliti Unit (Early-Middle Miocene); 5—Calcari a Briozoi e Litotamni (Middle Miocene); 6—Supersintema di Aielli-Pescina alluvial deposits (Pliocene–Pleistocene); 7—talus and alluvial
Image
A: Three-dimensional view and geological cross section for Colle Campetello...
in > Geology
Published: 01 June 2011
a Nummuliti e Discocycline (Early Paleocene); 3—Calcari a Miogypsine e Lepidocycline (Early-Middle Paleocene); 4—Calcari Spongoliti Unit (Early-Middle Miocene); 5—Calcari a Briozoi e Litotamni (Middle Miocene); 6—Supersintema di Aielli-Pescina alluvial deposits (Pliocene–Pleistocene); 7—talus and alluvial
Journal Article
Journal: PALAIOS
Published: 01 April 2016
PALAIOS (2016) 31 (4): 125–140.
... ). In the Apennine carbonate platforms the abundance of coralline algae clearly influenced regional lithostratigraphic nomenclature, e.g., “ Calcari a Briozoi e Litotamni ” ( Lithothamnion and Bryozoan Limestone) of the Latium–Abruzzi and Campano–Lucania Carbonate Platforms ( Carannante and Simone 1996 ; Brandano...
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Journal Article
Published: 23 December 2013
Italian Journal of Geosciences (2014) 133 (1): 85–100.
...-Abruzzi succession, represents carbonate ramp deposits (“Calcari a Briozoi e Litotamni fm.”; late Aquitanian to Serravallian/earliest Tortonian) ( C ivitelli & B randano , 2005 ; C arminati et alii , 2007 ). These ramp carbonates are generally overlain by a terrigenous succession where hemipelagic...
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