El Sabaya Formation In Bahariya

(PDF) Occurrence of barite mineralization in Bahariya

the Cretaceous Sabaya Formation occurring in El Bahariya Oasis, Northwestern Desert Field investigation and mineralogical studies were carried out in order to

Bahariya Formation Wikipedia

Extent The Bahariya Formation forms the base of the depression, the lower part of the enclosing escarpment and all of the small hills within The type section for the formation is found at Gebel ElDist, a hill at the northern end of the Bahariya depression Stratigraphy and sedimentology Four depositional sequences have been recognised in the Bahariya Formation in the Bahariya depression

Country: Egypt[PDF]

OCCURRENCE OF BARITE MINERALIZATION IN BAHARIYA

the Cretaceous Sabaya Formation occurring in El Bahariya Oasis, Northwestern Desert Field investigation and mineralogical studies were carried out in order to

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ASSESSMENT OF BAHARIYA HEMATITE BARITE ORE AS A

The Cretaceous rock succession (Sabaya, Bahariya, El Heiz and El Hafhuf Formations) comprises fluvialite to fluviomarine clastics of sandstone, claystone and shale The Sabaya Formation of Lower Cenomanian age (Morsy, 1987) 8 is coverd by Bahariya Formation which also belongs to the Lower Cenomanian (Soliman and El Badry, 1980) 9 The

Occurrence of barite mineralization in bahariya depression

Barite vein mineralization has been recorded South of Gebel El Haufhuf in the ground surface of El Bahariya depression, Western Desert of Egypt The barite veins that trend in different directions are actually associated with major fold and fault structures that are retricted to the oldest sandstone rock of the Sabaya Formation

Petroleum potential of the interpreted Paleozoic

In addition, gradations of the Sabaya Formation (the Kharita Formation) and of the Maghrabi Formation (the Bahariya Formation/El Heiz Member) may also occur The succession begins with clastic rocks of the Six Hills Formation that were deposited before the Aptian transgression and ends with the clastic Turonian Taref Formation

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Research Article Assessment of Bahariya Hematitebarite

The Cretaceous rock succession (Sabaya, Bahariya, El Heiz and El Hafhuf Formations) comprises fluvialite to fluviomarine clastics of sandstone, claystone and shale The Sabaya Formation of Lower Cenomanian age (Morsy, 1987) is coverd by Bahariya Formation which also belongs to the Lower Cenomanian (Soliman and El Badry, 1980)

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ASSESSMENT OF BAHARIYA HEMATITE BARITE ORE AS A

The Cretaceous rock succession (Sabaya, Bahariya, El Heiz and El Hafhuf Formations) comprises fluvialite to fluviomarine clastics of sandstone, claystone and shale The Sabaya Formation of Lower Cenomanian age (Morsy, 1987) 8 is coverd by Bahariya Formation which also belongs to the Lower Cenomanian (Soliman and El Badry, 1980) 9 The

Petroleum potential of the interpreted Paleozoic

In addition, gradations of the Sabaya Formation (the Kharita Formation) and of the Maghrabi Formation (the Bahariya Formation/El Heiz Member) may also occur The succession begins with clastic rocks of the Six Hills Formation that were deposited before the Aptian transgression and ends with the clastic Turonian Taref Formation

Occurrence of barite mineralization in bahariya depression

Barite vein mineralization has been recorded South of Gebel El Haufhuf in the ground surface of El Bahariya depression, Western Desert of Egypt The barite veins that trend in different directions are actually associated with major fold and fault structures that are retricted to the oldest sandstone rock of the Sabaya Formation

Structural setting and tectonic evolution of the Bahariya

To the southwest of Gebel El Hefhuf, the El HarraEl Hefhuf fault segment cuts the Bahariya Formation and on its southern side are three NEoriented, rightstepped en echelon folds Several NWoriented normal faults of short length and small throw are present in the northeastern part of Gebel El Hefhuf and indicate NESW lengthening

Formación Baharija Wikipedia, la enciclopedia libre

La Formación Baharija o Bahariya es una formación geológica, en el oasis del mismo nombre en Egipto Central Los sedimentos pertenecen al Cretácico superior, hace aproximadamente 95 millones de años, durante en CenomanienseLa presencia de fósiles de peces óseos en estos sedimentos sugiere un hábitat de tipo estuario sobre el antiguo mar de Tetis

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Mineralogical and geochemical investigations of the

part of the surrounding escarpment of El Bahariya Depression consist of Early Cenomanian clastic rocks of the Bahariya Formation The study area includes the Gabal GhorabiNasser (35 km2), El Harra (29 km 2), and El Gedida (65 km ) mine areas El Bahariya Depression is deformed by a NEtrending right

BahariyaFormation – Wikipedia

Die BahariyaFormation (auch Baharija, Bahariyya oder BahriyaFormation) ist ein siliziklastischer Schichtenverband, der während des Cenomaniums im nördlichen Ägypten abgelagert wurde Sie wurde erstmals 1914 von Ernst Stromer von Reichenbach unter der Bezeichnung „BaharijeStufe“ wissenschaftlich beschrieben Bekannt ist sie vor allem für ihre Wirbeltierfossilführung

Repeated occurrence of palaeowildfires during deposition

Aug 26, 2019· The Bahariya Oasis is situated in a morphological depression of an Eocene Limestone Plateau, where Cretaceous sediments are exposed It is located about 340 km southwest of Cairo in the Western Desert of Egypt (Fig 1)Within the area of the Bahariya Oasis, the oldest sediments exposed at the surface belong to the clastic unit of the Bahariya Formation, which is unconformably overlain by

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A reconstruction of the palaeoecology and environmental

nature of the El Heiz and G member beds The Bahariya formation (Fig 1) is divided into three members: Gebel Ghorabi, Gabel el Dist & El Heiz (Norton, 1967) and is succeeded by the Abu Roash formation (Beadnell, 1902); which is divided into several members, informally known by the initials A to G (Norton, 1967; Robertson Research International

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Reservoir Characterization for Bahariya Formation, Aman

152: Upper Bahariya Formation Bahariya formation is composed mainly of sandstone intercalated with shale, siltstone and limestone (Hantar, 1990)In the study area as in figure (14) represents neutrondensity cross plots of upper Bahariya formation It shows that the major lithology is sandstone and the average grain density (p R mat) R

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Journal of African Earth Sciences

Geological heritage of the Bahariya and Farafra oases, the central Western Desert, Egypt Ekaterina E Plyusnina a, Emad S Sallam b, Dmitry A Ruban a, *,1 a Department of Tourism, Higher School of Business, Southern Federal University, 23ja linija Street 43, RostovnaDonu, , Russia b Department of Geology, Faculty of Science, Benha University, Farid Nada Street 15, Benha 13518,

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Sequence stratigraphy of the Lower Cenomanian Bahariya

Sequence stratigraphy of the Lower Cenomanian Bahariya Formation, Bahariya Oasis, Western Desert, Egypt O Catuneanu a, MA Khalifa b, HA Wanas b,⁎ a Department of Earth and Atmospheric Sciences, University of Alberta, 126 Earth Sciences Building, Edmonton, Alberta, Canada T6G 2E3 b Geology Department, Faculty of Science, Menoufia University, Shebin ElKom, Egypt

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Repeated occurrence of palaeowildfires during deposition

Bahariya Formation, which is unconformably overlain by the late Campanian Hefuf Formation (Werner, 1990) The Bahariya Formation was defined by Said (1962)andElAkkad and Issawi (1963) According to Klitzsch and Hermina (1989), the Bahariya Formation at its type locality (and near our studied area) is lithologically composed of fluviatile

Petroleum potential of the interpreted Paleozoic

In addition, gradations of the Sabaya Formation (the Kharita Formation) and of the Maghrabi Formation (the Bahariya Formation/El Heiz Member) may also occur The succession begins with clastic rocks of the Six Hills Formation that were deposited before the Aptian transgression and ends with the clastic Turonian Taref Formation

Structural setting and tectonic evolution of the Bahariya

To the southwest of Gebel El Hefhuf, the El HarraEl Hefhuf fault segment cuts the Bahariya Formation and on its southern side are three NEoriented, rightstepped en echelon folds Several NWoriented normal faults of short length and small throw are present in the northeastern part of Gebel El Hefhuf and indicate NESW lengthening

Occurrence of barite mineralization in bahariya depression

Barite vein mineralization has been recorded South of Gebel El Haufhuf in the ground surface of El Bahariya depression, Western Desert of Egypt The barite veins that trend in different directions are actually associated with major fold and fault structures that are retricted to the oldest sandstone rock of the Sabaya Formation

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Mineralogical and geochemical investigations of the

part of the surrounding escarpment of El Bahariya Depression consist of Early Cenomanian clastic rocks of the Bahariya Formation The study area includes the Gabal GhorabiNasser (35 km2), El Harra (29 km 2), and El Gedida (65 km ) mine areas El Bahariya Depression is deformed by a NEtrending right

Formación Baharija Wikipedia, la enciclopedia libre

La Formación Baharija o Bahariya es una formación geológica, en el oasis del mismo nombre en Egipto Central Los sedimentos pertenecen al Cretácico superior, hace aproximadamente 95 millones de años, durante en CenomanienseLa presencia de fósiles de peces óseos en estos sedimentos sugiere un hábitat de tipo estuario sobre el antiguo mar de Tetis

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Reservoir Characterization for Bahariya Formation, Aman

152: Upper Bahariya Formation Bahariya formation is composed mainly of sandstone intercalated with shale, siltstone and limestone (Hantar, 1990)In the study area as in figure (14) represents neutrondensity cross plots of upper Bahariya formation It shows that the major lithology is sandstone and the average grain density (p R mat) R

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Repeated occurrence of palaeowildfires during deposition

Bahariya Formation, which is unconformably overlain by the late Campanian Hefuf Formation (Werner, 1990) The Bahariya Formation was defined by Said (1962)andElAkkad and Issawi (1963) According to Klitzsch and Hermina (1989), the Bahariya Formation at its type locality (and near our studied area) is lithologically composed of fluviatile

[PDF]

Journal of African Earth Sciences

Geological heritage of the Bahariya and Farafra oases, the central Western Desert, Egypt Ekaterina E Plyusnina a, Emad S Sallam b, Dmitry A Ruban a, *,1 a Department of Tourism, Higher School of Business, Southern Federal University, 23ja linija Street 43, RostovnaDonu, , Russia b Department of Geology, Faculty of Science, Benha University, Farid Nada Street 15, Benha 13518,

Repeated occurrence of palaeowildfires during deposition

Aug 26, 2019· The Bahariya Oasis is situated in a morphological depression of an Eocene Limestone Plateau, where Cretaceous sediments are exposed It is located about 340 km southwest of Cairo in the Western Desert of Egypt (Fig 1)Within the area of the Bahariya Oasis, the oldest sediments exposed at the surface belong to the clastic unit of the Bahariya Formation, which is unconformably overlain by

[PDF]

A reconstruction of the palaeoecology and environmental

nature of the El Heiz and G member beds The Bahariya formation (Fig 1) is divided into three members: Gebel Ghorabi, Gabel el Dist & El Heiz (Norton, 1967) and is succeeded by the Abu Roash formation (Beadnell, 1902); which is divided into several members, informally known by the initials A to G (Norton, 1967; Robertson Research International

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Evaluation of groundwater vulnerability in ElBahariya

Evaluation of groundwater vulnerability in ElBahariya Oasis, Western Desert, Egypt, using modelling and GIS techniques: A case study MHMasoud1,2 andMMElOsta3,∗ 1Hydrology Department, Desert Research Centre, El Matarya, Cairo, Egypt 2Water Research Centre, King Abdulaziz University, Jeddah, Saudi Arabia 3Geology Department, Faculty of Science, Damanhour University, Damanhour, Egypt

(PDF) Field Guide to the Bahariya Oasis | Waleed El Diasty

The base of the Bahariya Formation is unexposed, but inferred to be unconformable at the contact with the underlying basement (El Bassyouny, 1970), while its top shows an unconformable relationship with the overlying Upper Cenomanian El Heiz Formation (Figure 3; Khalifa and Abu ElHassan, 1993), or the LowerMiddle Eocene El Naqb Formation (El

Bahariyya – Wikipedia

AlBahariyya (arabisch الواحات البحرية alWahat alBahriyya, DMG alWāḥāt alBaḥriyya ‚die nördlichen Oasen‘) ist eine der fünf bedeutendsten bewohnten Senken im ägyptischen Teil der Libyschen WüsteSie liegt etwa 370 Kilometer südwestlich von KairoDie etwa ovale Senke erstreckt sich von Nordosten nach Südwesten, hat eine Länge von 94 km, eine maximale Breite

Lithofacies, cyclicity, diagenesis and depositional

Nov 01, 1993· ELHefhuf Formation r i 1 t BLHeiz FOrmatten j Baher~y~ Formation Upper Cretaceous /' Fold Fault Contact between rock units O Measured section t~ EL Gedida mine Fig 1 Geological map of the Bahariya Oasis (modified after Akkad and Issaw| (1963)