EN I Eocene molasse sediments from the Southern Carpathians (here the Conglomerate, in Romania) show some typical features of subaerial mass-flow deposits as coarse- to very coarse-grained lithofacies limited by multiple discontinuities, arranged in fining-upward cycles. Molasses sequences develop during the terminal stages of orogenic events. Fluvial and alluvial fans deposits are frequently identified asContinue reading “[TFM] Eocene molasse sediments from the Southern Carpathians”
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PETROCHRONICS 