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作 者:David Katemaunzanga Sinikiwe Ncube
机构地区:[1]Council for Geoscience [2]Geology Department,University of Fort Hare
出 处:《地学前缘》2009年第S1期259-260,共2页Earth Science Frontiers
摘 要:The Balfour Formation was subdivided into five members based on lithological variation that is characterized by alternating sandstone-and mudstone -dominated members.The sandstone dominated Oudeberg and Barberskrans members are composed of lithofacies that range from intraformational conglomerates to fine-grained sediments,whereas the mudstone dominated members(Daggaboersnek, Elandsberg and Palingkloof) are dominated by the fine-grained facies(Fm and F1).Petrography,geochemistry and palaeocurrent analysis indicated that the source rock of the Balfour Formation was to
关 键 词:Balfour Formation KAROO Supergroup Beaufort Group LITHOSTRATIGRAPHY sediment-tology PROVENANCE PERMO-TRIASSIC
分 类 号:P539[天文地球—古生物学与地层学]
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