Lateral distribution of detrital clay minerals in Lower Cretaceous sediment, western North Atlantic and its continental margin
Fine grained sediment from Lower Cretaceous turbidites (DSDP Site 603) and their correlative deltaic deposits (Baltimore Canyon Trough) were compared mineralogically and texturally. The shelf sediment is coarser grained than deep sea sediment and both are poorly sorted. Deltaic sediment is dominated...
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Format: | Text |
Language: | English |
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Online Access: | http://purl.flvc.org/fsu/lib/digcoll/etd/3161816 http://fsu.digital.flvc.org/islandora/object/fsu%3A78015/datastream/TN/view/Lateral%20distribution%20of%20detrital%20clay%20minerals%20in%20Lower%20Cretaceous%20sediment,%20western%20North%20Atlantic%20and%20its%20continental%20margin.jpg |