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Tectonic control is revealed in various ways (synsedimentary deformation structures, facies, architecture) in the coarse-grained delta systems that developed in the southeastern margin of the Guadix Basin, an intramontane basin in the central sector of the Betic Cordillera, Spain, during the late Tortonian (Miocene).Vertical trends in the architecture of the deltaic succession (230 m thick) show changes...
The deltaic succession in the Tabernas Basin represents the first deposition of marine sediments deposited during the late Tortonian transgression that linked the Mediterranean Sea to the Atlantic Ocean through the basins of the Betic Cordillera. The 100 m-thick succession consists of seven 5 to 20 m-thick vertically stacked wave-dominated Gilbert-type deltas. Towards the top of each unit, coral reef...
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