The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)

Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea durin...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Hendriks, Frits [verfasserIn] Kallenbach, Heinrich

Format:	Artikel
Sprache:	Englisch

Erschienen:	1986

Schlagwörter:	Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert

Anmerkung:	© Ferdinand Enke Verlag Stuttgart 1986

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Springer-Verlag, 1910, 75(1986), 2 vom: Juni, Seite 445-460
Übergeordnetes Werk:	volume:75 ; year:1986 ; number:2 ; month:06 ; pages:445-460

Links:	Volltext

DOI / URN:	10.1007/BF01820622

Katalog-ID:	OLC2070404528

Internformat


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allfields	10.1007/BF01820622 doi (DE-627)OLC2070404528 (DE-He213)BF01820622-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Hendriks, Frits verfasserin aut The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1986 Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert Kallenbach, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 75(1986), 2 vom: Juni, Seite 445-460 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:75 year:1986 number:2 month:06 pages:445-460 https://doi.org/10.1007/BF01820622 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 75 1986 2 06 445-460
spelling	10.1007/BF01820622 doi (DE-627)OLC2070404528 (DE-He213)BF01820622-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Hendriks, Frits verfasserin aut The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1986 Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert Kallenbach, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 75(1986), 2 vom: Juni, Seite 445-460 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:75 year:1986 number:2 month:06 pages:445-460 https://doi.org/10.1007/BF01820622 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 75 1986 2 06 445-460
allfields_unstemmed	10.1007/BF01820622 doi (DE-627)OLC2070404528 (DE-He213)BF01820622-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Hendriks, Frits verfasserin aut The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1986 Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert Kallenbach, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 75(1986), 2 vom: Juni, Seite 445-460 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:75 year:1986 number:2 month:06 pages:445-460 https://doi.org/10.1007/BF01820622 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 75 1986 2 06 445-460
allfieldsGer	10.1007/BF01820622 doi (DE-627)OLC2070404528 (DE-He213)BF01820622-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Hendriks, Frits verfasserin aut The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1986 Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert Kallenbach, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 75(1986), 2 vom: Juni, Seite 445-460 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:75 year:1986 number:2 month:06 pages:445-460 https://doi.org/10.1007/BF01820622 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 75 1986 2 06 445-460
allfieldsSound	10.1007/BF01820622 doi (DE-627)OLC2070404528 (DE-He213)BF01820622-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Hendriks, Frits verfasserin aut The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1986 Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert Kallenbach, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 75(1986), 2 vom: Juni, Seite 445-460 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:75 year:1986 number:2 month:06 pages:445-460 https://doi.org/10.1007/BF01820622 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 75 1986 2 06 445-460
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author	Hendriks, Frits
spellingShingle	Hendriks, Frits ddc 550 ssgn 13 misc Sandstone misc Maximum Extension misc Sedimentary Succession misc Lithostratigraphic Unit misc Western Desert The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)
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topic_title	550 VZ 13 ssgn The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt) Sandstone Maximum Extension Sedimentary Succession Lithostratigraphic Unit Western Desert
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title	The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)
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title_full	The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)
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title_sort	the offshore to backshore environments of the abu ballas formation of the se dakhla basin (western desert, egypt)
title_auth	The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)
abstract	Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. © Ferdinand Enke Verlag Stuttgart 1986
abstractGer	Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. © Ferdinand Enke Verlag Stuttgart 1986
abstract_unstemmed	Abstract The Abu Ballas Formation in the Western Desert of Egypt represents a marine intercalation within fluvial, Nubia-type sandstones. These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. They were accumulated on the western slope of the Kharga Uplift bounding the Dakhla Basin towards the east, which was partially flooded while the sea had its maximum extension. © Ferdinand Enke Verlag Stuttgart 1986
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title_short	The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)
url	https://doi.org/10.1007/BF01820622
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These deposits document an extensive transgression of Aptian age flooding the Dakhla Basin from north to south. Due to this first advance of the Tethyan sea during the Cretaceous, sediments of open and marginal marine provenance were accumulated in the SE of the basin. The sedimentary succession of the open marine facies is divided into five lithostratigraphic units which reflect that deposition was largely controlled by one single transgressive-regressive event. The transgressive sequence in the lower part of the formation comprises sandstones of a backshore to foreshore environment (unit 1) which are overlain by offshore claystones (unit 2). The middle portion of the sedimentary succession consists of silty and sandy strata (unit 3) which are attributed to large-scale redepositional processes due to intensified bottom currents during the maximum extension of the sea. These sediments are capped by offshore originated claystones (unit 4) grading upwards into siltstones and sandstones of transition-zone to backshore environments (unit 5), which indicate a gradual regression. This stratigraphic sequence documenting a retrograding-prograding shoreline due to the transgression and regression of the Aptian sea, interfingers with silty and sandy deposits of the marginal marine facies of the Abu Ballas Formation. Comparable to the lithostratigraphic units 1 and 5 these strata represent a variety of sedimentary environments ranging from the backshore to the transition zone. 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The offshore to backshore environments of the Abu Ballas Formation of the SE Dakhla Basin (Western Desert, Egypt)

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