Mass-transport deposits from the Toarcian of the Umbria-Marche-Sabina Basin (Central Italy)

Cipriani, Angelo; Zuccari, Costantino; Innamorati, Giulia; Marino, Maria; Petti, Fabio Massimo

doi:10.3301/ijg.2019.14

Cited by 7 publications

(3 citation statements)

References 86 publications

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“…The computed slip rates are in the order of 600 m/Myr, but values of 1000 m/Myr cannot be excluded. Although this statement must encompass the possibility that episodes of minor fault‐zone rejuvenation, documented in the Umbria‐Marche‐Sabina region (Toarcian: Cipriani et al., 2020; early Bajocian: Galluzzo & Santantonio, 2002; Cannata, 2007), can have occurred locally, we must conclude that the greater part (post‐early Sinemurian) of the infilling of rift basins in this region took place in a post‐rift regime.…”

Section: Discussionmentioning

confidence: 99%

Constraining the slip rate of Jurassic rift faults through the drowning history of a carbonate platform

et al. 2021

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“Classic” field mapping in sedimentary successions, where lithostratigraphy, biostratigraphy and sedimentology meet, still has potential for producing answers to long‐standing problems in basin analysis. In the Northern Apennines of Italy, constraints on the slip rates of Early Jurassic rift faults, related to the embryonic separation of Eurasia and Gondwana, are provided by sedimentology and ammonite biostratigraphy, coupled with the field mapping of exposed tracts of the submarine escarpments and of the clinoform slopes which bordered carbonate footwall blocks. Slip rates of 600–1,000 m/Myr are here computed for Tethyan rift faults, producing >1 km of palaeostructural relief in ~2 million years (earliest Sinemurian: Bucklandi p.p. – Semicostatum p.p. zones).

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Section: Discussionmentioning

confidence: 99%

Constraining the slip rate of Jurassic rift faults through the drowning history of a carbonate platform

et al. 2021

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“…The Sabina Basin hosted small‐scale intrabasinal highs (e.g. Mt Rosato, Polino, Mt Macchialavela‐Mt Pallaroso and Mt Borragine PCPs—Capotorti et al, 2018; Cipriani, Zuccari, Innamorati, Marino, & Petti, 2020; Damiani et al, 1991; Leonardi, Lipparini, Nicosia, Ursini, & Varazi, 1997), as well as the huge Sabina Plateau (Galluzzo & Santantonio, 2002) during the Jurassic (see Figure 11). The latter constituted the western boundary of the Sabina Basin.…”

Section: Discussionmentioning

confidence: 99%

Geological mapping reveals the role of Early Jurassic rift architecture in the dispersal of calciturbidites: New insights from the Central and Northern Apennines

2020

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The role of sea-bottom topography in the dispersal of shallow water-derived calciturbidites across a submarine rift, as determined by the local extensional architecture, is under-investigated, namely with pelagic settings along ancient passive continental margins. A comparison with modern carbonate platform/basin analogues, or with siliciclastic systems, is not always feasible, as ancient carbonate systems were commonly home to anachronistic environments (e.g. the Western Tethyan Mesozoic). Our study focuses on: (a) a reconstruction of the palaeotectonic architecture of the 1486 | EAGE CIPRIANI et Al.

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“…By contrast, pelagic environments developed on the hangingwall blocks of rift faults. This is the case of the well-known Umbria-Marche-Sabina (Centamore et al, 1971;Cantelli et al, 1978;Farinacci et al, 1981;Corda & Mariotti, 1986;Cecca et al, 1990;Cosentino & Parotto, 1992;Santantonio, 1993Santantonio, , 1994Galluzzo & Santantonio, 2002;Rusciadelli et al, 2009;Santantonio & Carminati, 2011;Rusciadelli & Ricci, 2013;Cipriani, 2016Cipriani, , 2019Fabbi et al, 2016;Romano et al, 2018Romano et al, , 2019aRomano et al, , 2019bCipriani & Bottini, 2019aCitton et al, 2019Citton et al, , 2020Cipriani et al, 2019Cipriani et al, , 2020aCipriani et al, , 2020b and Molise-Lagonegro (Ghisetti & Vizzani, 1998;Festa et al, 2006) basins surrounding the Apennine Carbonate Platform. The neritic environments passed to the surrounding pelagic basins through tectonic-related slopes/margins (Praturlon, 1968;Parotto, , 1971Cantelli et al, 1978).…”

Section: Geological Settingmentioning

confidence: 99%

The dolines of Campoli Appennino (Frosinone, Italy): a geo-historical overview

Cipriani¹,

Roncacè²

2020

ROL

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The spectacular karst morphologies of the area between Campoli Appennino and Alvito (Southern Lazio, Italy) represent an emblematic example of karst processes acting on different types of substrate. Hypogean forms are subordinated to epigean ones, with dolines as undiscussed leaders. Imposing and famous are the dolines of "Fossa Maiura" (also known as "Fossa Majura" or "Fossa Majora") and "Il Tomolo", around which the town of Campoli Appennino is built in a semi-circle, but are 8 the karst depressions with a diameter greater than 200 m ("main macrodolines") in this area. These forms of landscape controlled the cultural and socio-economic aspects of this corner of Ciociaria. Starting from the second half of the 19th century, the hydrogeological, structural, stratigraphic and geomorphological features of the Campoli Appennino area, attracted the interest of geologists, allowing to recognize a "site of geological memory". However, the geological heritage of this area worth greater visibility, as indicated by the poorly-developed geo-tourism, and for a greater dissemination, making the geo-morphological features more accessible and understandable, even for non-geologists.

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Mass-transport deposits from the Toarcian of the Umbria-Marche-Sabina Basin (Central Italy)

Cited by 7 publications

References 86 publications

Constraining the slip rate of Jurassic rift faults through the drowning history of a carbonate platform

Constraining the slip rate of Jurassic rift faults through the drowning history of a carbonate platform

Geological mapping reveals the role of Early Jurassic rift architecture in the dispersal of calciturbidites: New insights from the Central and Northern Apennines

The dolines of Campoli Appennino (Frosinone, Italy): a geo-historical overview

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