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The Promina Beds in northern Dalmatia are a more than 2000 m thick calciclastic succession of Middle Eocene–Early Oligocene age, constituting the infill of the piggyback part of the Dinaric Foreland Basin (Fig. A, B ; MRINJEK et al., 2011 ; ĆOSOVI
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::0a29535e5abdaf118a6ef3eb338bf4fc
https://www.bib.irb.hr/1026880
https://www.bib.irb.hr/1026880
Little is known about controls of clastic deposition in deep limestone caverns, particularly those with no known connection with the surface. Such caverns are occasionally discovered by tunneling, but seldom studied in detail. One of several caverns
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::1dc31f1bfa5e7e6a9f898569c2c00869
https://www.bib.irb.hr/944447
https://www.bib.irb.hr/944447