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San Cassiano Formation
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San Cassiano Formation : ウィキペディア英語版
San Cassiano Formation

San Cassiano Formation (Anisian-Carnian) is a geologic formation located on the Southern Alps (Northeast of Italy) in the Dolomites. These Triassic dolomites are considered to be a classic example of ancient carbonate platforms.〔(Bosellini, A., Gianolla, P., & Stefani, M. (2003). Geology of the dolomites. Episodes, 26(3). )〕 As the allochthonous elements in the Shale strata (Cipit boulders) show a good preservation, fossils and microbialites contained in these elements are useful in detailed geochemical analyses.〔(F., & Lopez‐Esquivel, L. (2011). Análisis geoquímico (elementos mayores, menores, traza, δ13C, δ18O y tierras raras) de microbialitas selectas provenientes de la Formación Fan Casiano (Triásico Medio ‐ Superior, NE de Italia). Boletín de la Sociedad Geológica Mexicana, 63(3), 399–420. )〕
==History==
Research on the San Cassiano Formation started in the 19th century with the works of Nicolas de Saussure and the stratigraphic works of Leopold von Buch and Alexander von Humboldt.〔(Nomination of the dolomites for inscription on the world natural heritage list UNESCO. Online. URL http://www.dolomiti‐unesco.org/ )〕 By the late 19th century Richthofen and von Mojsisovics had already acknowledge the reefal origin of these mountains.〔

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