2019
DOI: 10.1007/s12517-019-4362-8
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Grain size and mineralogical characteristics of the stream sediments, east of Abu Zeneima area, southwestern Sinai, Egypt

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Cited by 4 publications
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“…The entire Paleozoic succession unconformably overlies the Precambrian basement rocks (gneisses and younger granites) and unconformably underlies the Permo-Triassic sandstone and mudstone red beds. The Abu Thora Formation in certain places is capped by basaltic sheets (Mesozoic), and it is also dissected by doleritic and basaltic dykes [34,35].…”
Section: Sample Collection and Preparationmentioning
confidence: 99%
“…The entire Paleozoic succession unconformably overlies the Precambrian basement rocks (gneisses and younger granites) and unconformably underlies the Permo-Triassic sandstone and mudstone red beds. The Abu Thora Formation in certain places is capped by basaltic sheets (Mesozoic), and it is also dissected by doleritic and basaltic dykes [34,35].…”
Section: Sample Collection and Preparationmentioning
confidence: 99%