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Wanas, H.A (2002) Petrography, geochemistry and primary origin of spheroidal dolomite from the Upper Cretaceous/Lower Tertiary Maghra El-Bahari Formation at Gabal Ataqa, Northwest Gulf of Suez, Egypt. Sedimentary Geology, 151 (3) 211-224 doi:10.1016/s0037-0738(01)00258-5

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Reference TypeJournal (article/letter/editorial)
TitlePetrography, geochemistry and primary origin of spheroidal dolomite from the Upper Cretaceous/Lower Tertiary Maghra El-Bahari Formation at Gabal Ataqa, Northwest Gulf of Suez, Egypt
JournalSedimentary Geology
AuthorsWanas, H.AAuthor
Year2002 (August)Volume151
Issue3
PublisherElsevier BV
DOIdoi:10.1016/s0037-0738(01)00258-5Search in ResearchGate
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Mindat Ref. ID553630Long-form Identifiermindat:1:5:553630:0
GUID0
Full ReferenceWanas, H.A (2002) Petrography, geochemistry and primary origin of spheroidal dolomite from the Upper Cretaceous/Lower Tertiary Maghra El-Bahari Formation at Gabal Ataqa, Northwest Gulf of Suez, Egypt. Sedimentary Geology, 151 (3) 211-224 doi:10.1016/s0037-0738(01)00258-5
Plain TextWanas, H.A (2002) Petrography, geochemistry and primary origin of spheroidal dolomite from the Upper Cretaceous/Lower Tertiary Maghra El-Bahari Formation at Gabal Ataqa, Northwest Gulf of Suez, Egypt. Sedimentary Geology, 151 (3) 211-224 doi:10.1016/s0037-0738(01)00258-5
In(2002, August) Sedimentary Geology Vol. 151 (3) Elsevier BV

See Also

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Wanas, H.A., Abu El-Hassan, M.M. (2006) Paleosols of the Upper Cretaceous–Lower Tertiary Maghra El-Bahari Formation in the northeastern portion of the Eastern Desert, Egypt: Their recognition and geological significance. Sedimentary Geology, 183 (3) 243-259 doi:10.1016/j.sedgeo.2005.09.013
Wanas, H.A., Sallam, E. (2016) Abiotically-formed, primary dolomite in the mid-Eocene lacustrine succession at Gebel El-Goza El-Hamra, NE Egypt: An approach to the role of smectitic clays. Sedimentary Geology, 343. 132-140 doi:10.1016/j.sedgeo.2016.08.003
Sallam, E.S., Wanas, H.A. (2019) Petrography and geochemistry of the Jurassic siliciclastic rocks in the Khashm El-Galala area (NW Gulf of Suez, Egypt): Implication for provenance, tectonic setting and source area paleoweathering. Journal of African Earth Sciences, 160. 103607 doi:10.1016/j.jafrearsci.2019.103607
McKay, J.L., Longstaffe, F.J. (2003) Sulphur isotope geochemistry of pyrite from the Upper Cretaceous Marshybank Formation, Western Interior Basin. Sedimentary Geology, 157 (3) 175-195 doi:10.1016/s0037-0738(02)00233-6
Heydari, E., Hassanzadeh, J., Wade, W.J. (2001) Corrigendum to “Geochemistry of central Tethyan Upper Permian and Lower Triassic strata, Abadeh region, Iran” [Sedimentary Geology 137 (2000) 85–99]. Sedimentary Geology, 143 (3) 329 doi:10.1016/s0037-0738(01)00124-5
Yoshida, S (2000) Sequence and facies architecture of the upper Blackhawk Formation and the Lower Castlegate Sandstone (Upper Cretaceous), Book Cliffs, Utah, USA. Sedimentary Geology, 136 (3) 239-276 doi:10.1016/s0037-0738(00)00104-4
Ray, Sanghamitra, Chakraborty, Tapan (2002) Lower Gondwana fluvial succession of the Pench–Kanhan valley, India: stratigraphic architecture and depositional controls. Sedimentary Geology, 151 (3) 243-271 doi:10.1016/s0037-0738(01)00260-3
Abdel-Wahab, Antar A. (1992) Provenance of Gebel El-Zeit sandstones, gulf of Suez, Egypt. Sedimentary Geology, 75 (3) 241-255 doi:10.1016/0037-0738(92)90095-9
Hamed Metwalli, M., Wali, A.M.A., Abd El-Shafy, A. (1987) Cretaceous petroleum-bearing rock types—their diagenesis and significance in the Gulf of Suez area, Egypt. Sedimentary Geology, 53 (3) 269-304 doi:10.1016/0037-0738(87)90038-8
Zhu Jingquan, (1998) Characteristics and origin of polycrystalline dolomite needles in the Triassic Jialingjiang Formation, Upper Yangtze Platform, southwest China. Sedimentary Geology, 118 (1) 119-126 doi:10.1016/s0037-0738(98)00008-6
El Albani, Abderrazzak, Cloutier, Richard, Candilier, Anne-Marie (2002) Early diagenesis of the Upper Devonian Escuminac Formation in the Gaspé Peninsula, Québec: sedimentological and geochemical evidence. Sedimentary Geology, 146 (3) 209-223 doi:10.1016/s0037-0738(01)00119-1
 
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