Calcare di Aurisina

Calcari di Aurisina
Stratigraphic range: Santonian-Campanian
~84–70.6 Ma
Aurisina quarries being exploited
TypeGeological formation
Sub-unitsZolla member
AreaFriuli-Venezia Giulia
Lithology
PrimaryLimestone
Location
Coordinates45°48′N 13°36′E / 45.8°N 13.6°E / 45.8; 13.6
Approximate paleocoordinates23°30′N 16°12′E / 23.5°N 16.2°E / 23.5; 16.2
RegionTrieste
Country
Type section
Named forAurisina
Calcare di Aurisina is located in Italy
Calcare di Aurisina
Calcare di Aurisina (Italy)

The Calcare di Aurisina (Also known as Aurisina Formation, “Formazione di Monrupino”, Trieste Karst Limestone formation, “Repen formation”, “Sežana formation” and “Lipiza formation”)[1][2][3] is a Mesozoic geologic formation in Italy and Slovenia.[3] This limestones are found in the Trieste area and are of Late Cretaceous (Santonian-Campanian) age, being a local record of Carbonate platform limestones, historically quarried by cutting large blocks using steel wire, what has allowed more access to them, as numerous quarries allow excellent exposure.[3][4] Due to being cut into large blocks and slabs, that usually end stored near the quarries, detailed, three-dimensional study of the rock's composition and fossils can be easily done.[5][6]

  1. ^ Consorti, Lorenzo; Arbulla, Deborah; Bonini, Lorenzo; Fabbi, Simone; Fanti, Federico; Franceschi, Marco; Frijia, Gianluca; Pini, Gian Andrea (2021). "The Mesozoic palaeoenvironmental richness of the Trieste Karst". Geological Field Trips. 13 (2.2): 1–40. doi:10.3301/gft.2021.06. hdl:11368/3009529. ISSN 2038-4947.
  2. ^ Cucchi, Franco; Forti, Fabio; Finocchiaro, Furio (1987). "Carbonate surface solution in the classical karst". International Journal of Speleology. 16 (3/4): 125–138. doi:10.5038/1827-806x.16.3.6. ISSN 0392-6672.
  3. ^ a b c Jurkovšek, Bogdan; Biolchi, Sara; Furlani, Stefano; Kolar-Jurkovšek, Tea; Zini, Luca; Jež, Jernej; Tunis, Giorgio; Bavec, Miloš; Cucchi, Franco (2016-08-12). "Geology of the Classical Karst Region (SW Slovenia–NE Italy)". Journal of Maps. 12 (sup1): 352–362. Bibcode:2016JMaps..12S.352J. doi:10.1080/17445647.2016.1215941. hdl:11368/2888161. ISSN 1744-5647.
  4. ^ Sanders, D (2001). "Burrow-mediated carbonate dissolution in rudist biostromes (Aurisina, Italy): implications for taphonomy in tropical, shallow subtidal carbonate environments". Palaeogeography, Palaeoclimatology, Palaeoecology. 168 (1–2): 39–74. Bibcode:2001PPP...168...39S. doi:10.1016/s0031-0182(00)00249-2. ISSN 0031-0182.
  5. ^ Castracane degli Antelminelli, Francesco (1886). Analisi microscopica di un Calcare del Territorio di Spoleto. Roma: Tipografia delle scienze matematiche e fisiche. doi:10.5962/bhl.title.64225.
  6. ^ Venturini, S.; Tentor, M. (2010). "La Breccia di Slivia: Una testimonianza di eventi paleotettonici campaniano-maastrichtiani nel Carso Triestino" (PDF). Natura Nascosta. 41 (6): 1–15.