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In the Middle Adriatic deep off-shore wells the following sedimentaryfaciess exist: fenestral and Charophyte limestone facies (X); facies of foraminiferal wackestone-packstone, ostracod marls and fine grained breccia conglomerate (A): facies of foraminiferal packstonegrainstone (B) and miliolidal mudstone-wackestone (C): facies of porous limestone?, grainstone? (Y): facies of fossiliferous mudstonepackstone (D); algal bound stone/bindstone and wackestone facies (E): facies of the foraminiferaldoi:10.4154/gc.1997.05 doaj:42be132a6e2e4cda9a4b702ab620ca79 fatcat:y5zyyatd25d7he2t6mn3tisw2q