Architecture and sedimentary facies evolution of a marine, expanding outer‐arc half‐graben (Crete, late Miocene)

Abstract

AbstractVertical trends in architecture and facies of delta systems are preserved in a clastic wedge of an expanding marine half‐graben in which tectonics, eustatic sea‐level change and climatic change are roughly known from independent evidence. The studied half‐graben is situated on Crete (Greece) and part of a larger, E‐W‐trending extensional domain situated north of the Hellenic subduction zone. The extension seems to be related to the southward migration of the trench (roll‐back) in early Late Miocene times. The infill pattern is discussed in the light of theoretical fault‐growth models for expanding half‐grabens.The geometry of the half‐graben fill is typically wedge shaped, with a thickness of nearly 1000 m near the fault scarp thinning to c. 50 m about 20 km away from the scarp. The lower part of the wedge (Stratified Prina Series) contains coarsening‐upward units representing progradational, shallow‐marine deltas. At the base of the wedge these units are thin and retrogradationally stacked. Upwards in the succession, the units become composite (coarsening‐upward subunits), thicker and finer grained. The composite structure, the thickening and the fining trend is related to progressive increase in accommodation space inherent in fault growth.Rapid deepening of the basin from the photic zone (evidenced by intercalated coral and stromatolite beds) up to a depth of 900 m started at the top of the Stratified Prina Series. The deepening continued over some tens of metres of marly sediments of the base of the Kalamavka Formation and may be related to structural collapse of the fault block. After the structural collapse, basin depth remained more or less constant and basin infilling occurred by progradation of deep‐water delta systems. These systems are characterized by a muddy delta slope with channelized conglomerates, and by mainly aggradation of prodelta turbidites deposited in small lobes at the base of slope.