Dabrio González, Cristino JoséPolo Camacho, Dolores2023-06-202023-06-2019950213-683Xhttps://hdl.handle.net/20.500.14352/56817A brief description of detail stratigraphy of the Late-Neogene Terminal Carbonate Complex and the Sorbas Member, and the precise role of the stromatolite layers that occur interbedded. The vicinity to the sources of coarse-gained sediment imput, mobility of the sea-bottom, and the topographic elevation reached by the sea during high stands of 4th/5th order oscillations control the development of stromatolites. Recognition of high-frequency (fourth and fifth-order cycles) inside a third-order (TB 3.4) eustatic cycle.spajournal articlehttp://www.sociedadgeologica.es/publicaciones_geogaceta.htmlopen access551.7(460.358)Mixed shelfFringing reefsStromatolitesTalus slopeEustatic oscillationsLate NeogeneSouth-eastern SpainGeología estratigráfica2506.19 Estratigrafía