Stratigraphic column for gulf of suez, western desert and nile delta, egypt (the simplest for students) m.m.badawy
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Stratigraphic column for gulf of suez, western desert and nile delta, egypt (the simplest for students) m.m.badawy
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Stratigraphic column for gulf of suez, western desert and nile delta, egypt (the simplest for students) m.m.badawy
- 1. Eon Era Period Epoch Recent (Holocene) Epoch Pleistocene Pliocene Gulf of Suez Seal , (rock salts) Western Desert Stratigraphic Column for Gulf of Suez, Western Desert and Nile Delta, Egypt (The Simplest for Students) Quaternary Post-Zeit Kareem Seal, (rock salts, anhydrite with shale interbeds) Seal , (gypsum and anhydrite with shale interbeds) Nile Delta Marmarica Recent (Holocene) Pleistocene Bilqas / Mit Ghamr El-Wastani Post-Rift Zeit South Gharib Belayim Ras Malaab Group Oligocene Eocene Paleocene Syn-Rift (Lower Miocene) Phanerozoic Cenozoic Tertiary Thebes Esna-Shale Rudies Nukhul Reservoir , (basal miocene age, represented by reefal limestone in some areas and clastic sequence in another areas from the gulf of suez) Reservoir, (middle eocene age, represented by cherty and flinty limestone) Source , (Paleocene) Apollonia Dabaa Moghra Source , (E,F and G), Reservoirs, (G,F,D,C,B) late cenomanian, is considered the second main reservoir rocks in the western desert, it contains dolomite and limestone beds, (G, with porosity 10-35% and the oil is 45 API), (F, produced heavy Miocene Pliocene Kafr El-Sheikh Abu-Madi Khoman Abo Roash (A to G) Source , (Lower Miocene Shale), And Reservoir , sandstone interbeds with shale intervals forming lenses of stratigraphic traps in many of oil fields)Phanerozoic Mesozoic Cretaceous Matulla Brown-Limestone Source , (Upper Cretaceous) Miocene Alamein Alam El-Bueib and the oil is 45 API), (F, produced heavy oil (crude) with 15 API) (D, produced oil with 36 API), (C, contains sandstone and produce oil 32 API in Abu Gharadig and Abu Sanan Fields) Reservoir , (cenomanian, contains good reservoirs with porosity 18-25%, about 90% from oil and gas fields are produced from the bahariya as(Razzak, Khalda, Meleiha, Salam, Amar, Yasser, Zahra, Tut, Horous and Lotus Fields), these oil fields produced oil of about 34 to 50 degree API Reservoir, (good potential reservoir rock, oil bearing in Salum and Abu Gharadig Fields) Reservoir , (hard and dense vuggy dolomite of porosity 3-12% , oil bearing in Alamein, Yidma and Razzak Field) Source, (Lower Cretaceous), and Reservoir, (contained fine grained sandstone which act as a good reservoir Bahariya Kharita Dahab Pre-Rift Qawasim Sidi Salim Basement Source , (Jurassic) Created By: Proterozoic(Precambrian) Nubia-A Paleozoic Triassic Jurassic Masajid Khatatba Yakout Ras Qattara Shifah Reservoir , (consists of porous and permeable and sandstone) Source , (Lower Carboniferous) Reservoir, (consists of porous and permeable and sand stone)Nubia-C Nubia-B Basement Oligocene Alam El-Bueib Qantara sandstone which act as a good reservoir rock, produced oil and gas in Umbaraka, Hayat, Safir and Tut Fields) Wadi El-Natrun Dabaa Eocene Apollonia Jurassic Masajid Khatatba Mahmoud Mostafa Badawy, (Demonstrator of Geophysics, Geology Department, Faculty of Science, Alexandria University, Egypt)