Abstract: Sedimentary environment and tectonic deformations of the Neoproterozoic Iron formation at the Wadi El-Dabbah greenstone sequence, Central Eastern Desert, Egypt (2017 AGU Fall Meeting)

Sedimentary environment and tectonic deformations of the Neoproterozoic Iron formation at the Wadi El-Dabbah greenstone sequence, Central Eastern Desert, Egypt

Shoichi Kiyokawa¹, Taishi Suzuki², Minoru Ikehara³, Kenji Horie⁴, Mami Takehara⁴, Hanna Abd-Elmonem⁵, Al-Dekouny Maher Dawoud⁶ and Mohamed Mahmoud El-Hasan⁵, (1)Kyushu University, Department of Earth and Planetary Science, Fukuoka, Japan, (2)Kyushu University, Fukuoka, Japan, (3)Kochi University, Center of Advanced Marine Core Research, Kochi, Japan, (4)NIPR National Institute of Polar Research, Tokyo, Japan, (5)Menoufiya University, Geology Dept., Faculty of Science, Menoufiya, Egypt, (6)Menoufiya University, Geology Dept., Faculty of Science,, Menoufiya, Egypt

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