Upper Miocene Karst Collapse Structures of the East Coast, Mallorca, Spain

V obalnih stenah na Mallorci (Zahodno Sredozemlje) so obsežni izdanki zgornjemiocenskih karbonatnih kamnin. Na vzhodni obali otoka prekrivajo grebenski sklop mesinijski plitvovodni karbonati. Tod so v zgornjemiocenskih kamninah stevilne paleokraske podorne strukture. V apnence Santanyi so vrezane strukture v obliki crke V, kar kaže na udiranje stropov jam, nastalih v spodaj ležecih grebenskih sklopih. Glede na model je mogoce nastanek nekaterih izmed teh kraskih podornih struktur povezati z zgodnjimi diagenetskimi procesi, na katere so vplivale pogoste spremembe nivoja morske gladine. V casu nizkega nivoja morske gladine je sladkovodni tok izdolbel jamski sistem v bližini vodne gladine na tak nacin, da je raztapljal aragonit v frontalnem faciesu in skupke koral v obstojecih lagunskih plasteh. Ta jamski sistem se je razvijal v bližini povrsinske erozijske baze. Med kasnejsim dvigom morske gladine so plasti notranjega dela selfa prekrile predhodno zakraselo jedro grebena in izvenlagunske plasti. Vrezane »V« strukture je lahko povzrocila povecana teža odloženih plitvovodnih karbonatov, zaradi cesar je prihajalo do gravitacijskih udiranj jamskih stropov v casu, ko te plasti se niso bile popolnoma strjene. In the sea cliffs on the Mallorca Island, Western Mediterranean there are extensive outcrops of Upper Miocene carbonate rocks. On the Eastern coast of Mallorca, the reefal complex is overlain by a Messinian shallowwater carbonate complex. There are abundant Paleokarst collapse structures. The Santanyi Limestone beds are affected by V-incasion structures produced by roof collapse of caverns developed in the underlying reefal complex. According to the model, the origin of some of these karst-collapse structures may be related to early diagenetic processes controlled by high-frequency sea-level fluctuations. During lowstands of sea level, freshwater flow might have create a cave system near the water table by dissolution of aragonite in the reef front facies and coral patches existing in the lagoonal beds. This cave system developed near the subaerial erosion surface. During subsequent rise of sea level inner-shelf beds overlaid the previously karstified reef-core and outer-lagoonal beds. Increase of loading by subsequent accretion of the shallow-water carbonates might have produced V-incasion structures by gravitational collapse of cave roofs when these beds were still not completely consolidated.