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Rt Kamenjak, koji se nalazi na samom jugu Istre, građen je od cenomanskih i turonskih plitkovodnih karbonata taloženih na Jadranskodinaridskoj karbonatnoj platformi. Cenomanske naslage javljaju se na sjeverozapadnom dijelu obale i ukazuju na taložne okoliše plitkog subtajdala i karbonatne rampe. Turonske naslage grade ostatak rta, s time da turonske naslage dijelimo na tri jedinice, od kojih su dvije taložene u plitkovodnim peritajdalnim okolišima, a jedna je taložena u okolišu potopljene platforme na granici cenomanturon. Kamenjak promontory is situated on the very south of Istrian peninsula and is composed of Cenomanian and Turonian shallowmarine carbonates deposited on AdriaticDinaridic Carbonate Platform. Cenomanian deposits occur on the northwestern part of the promontory and indicate shallow subtidal and carbonate ramp environments. Turonian deposits make the rest of the promontory and their succession can be divided into three units. The first one was deposited in environments of the drowned platform, while the second and third are deposited in reestablished shallowwater environment. |
