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Статья

Evaporite karst in Italy: a review

Jo De WaeleUniversity of BolognaLéonardo PicciniUniversity of FlorenceAndrea ColumbuUniversity of MelbourneGiuliana MadoniaUniversity of PalermoMarco VattanoUniversity of PalermoChiara CalligarisTrieste UniversityIlenia M. D’AngeliUniversity of BolognaMario PariseDepartment of Earth and Geo-Environmental Sciences, Università "Aldo Moro", Bari, ItalyMauro ChiesiSocietà Speleologica Italiana, Via Zamboni 67, 40126 Bologna, ItalySocietà Speleologica ItalianaSocietà Speleologica Italiana, Via Zamboni 67, 40126 Bologna, ItalyMichele SivelliPolytecnic university of TurinSocietà Speleologica ItalianaUniversità degli studi di Trieste = University of TriesteBartolomeo VignaAlma Mater Studiorum Università di Bologna = University of BolognaLuca ZiniAlma Mater Studiorum Università di Bologna = University of BolognaVeronica ChiariniUniversity of BolognaSauro, FrancescoUniversity of BolognaRussell N. DrysdaleUniversity of MelbournePaolo FortiUniversity of Bologna
2017en
ABI

Аннотация

Although outcropping rarely in Italy, evaporite (gypsum and anhydrite) karst has been described in detail since the early 20th century. Gypsum caves are now known from almost all Italian regions, but are mainly localised along the northern border of the Apennine chain (Emilia Romagna and Marche), Calabria, and Sicily, where the major outcrops occur. Recently, important caves have also been discovered in the underground gypsum mines in Piedmont. During the late 80s and 90s several multidisciplinary studies were carried out in many gypsum areas, resulting in a comprehensive overview, promoting further research in these special karst regions. More recent and detailed studies focused on the gypsum areas of Emilia-Romagna and Sicily. Sinkholes related to Permian-Triassic gypsum have been studied in Friuli Venezia Giulia. This article reviews the state of the art regarding different aspects of evaporite karst in Italy focusing on the main new results.

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