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- W2205231811 abstract "In the alluvial part of the Promina beds of northern Dalmatia (Late Eocene to possible Early Oligocene age) the main, SW-ward paleocurrent pattern was determined from clast orientation measurements within massive and flat-bedded conglomerates. Preferred clast fabric, facies characteristics, and downward transition into shoreline and shallow-marine sandstone and conglomerate suggest a prograding, braid delta system." @default.
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- W2205231811 date "1993-06-10" @default.
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- W2205231811 title "Conglomerate Fabric and Paleocurrent Measurement in the Braided Fluvial System of the Promina Beds in Northern Dalmatia (Croatia)" @default.
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- W2205231811 doi "https://doi.org/10.4154/gc.1993.10" @default.
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