A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains

Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is dif...
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Gespeichert in:

Autor*in:	Jossen, J. -A. [verfasserIn] Filali-Moutei, J.

Format:	Artikel
Sprache:	Englisch

Erschienen:	1992

Schlagwörter:	Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain

Anmerkung:	© Ferdinand Enke Verlag Stuttgart 1992

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Springer-Verlag, 1910, 81(1992), 1 vom: Feb., Seite 143-156
Übergeordnetes Werk:	volume:81 ; year:1992 ; number:1 ; month:02 ; pages:143-156

Links:	Volltext

DOI / URN:	10.1007/BF01764545

Katalog-ID:	OLC2070407853

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520			\|a Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin.
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allfields	10.1007/BF01764545 doi (DE-627)OLC2070407853 (DE-He213)BF01764545-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Jossen, J. -A. verfasserin aut A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1992 Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain Filali-Moutei, J. aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 81(1992), 1 vom: Feb., Seite 143-156 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:81 year:1992 number:1 month:02 pages:143-156 https://doi.org/10.1007/BF01764545 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_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 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_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_4193 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4325 GBV_ILN_4337 AR 81 1992 1 02 143-156
spelling	10.1007/BF01764545 doi (DE-627)OLC2070407853 (DE-He213)BF01764545-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Jossen, J. -A. verfasserin aut A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1992 Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain Filali-Moutei, J. aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 81(1992), 1 vom: Feb., Seite 143-156 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:81 year:1992 number:1 month:02 pages:143-156 https://doi.org/10.1007/BF01764545 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_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 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_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_4193 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4325 GBV_ILN_4337 AR 81 1992 1 02 143-156
allfields_unstemmed	10.1007/BF01764545 doi (DE-627)OLC2070407853 (DE-He213)BF01764545-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Jossen, J. -A. verfasserin aut A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1992 Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain Filali-Moutei, J. aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 81(1992), 1 vom: Feb., Seite 143-156 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:81 year:1992 number:1 month:02 pages:143-156 https://doi.org/10.1007/BF01764545 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_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 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_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_4193 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4325 GBV_ILN_4337 AR 81 1992 1 02 143-156
allfieldsGer	10.1007/BF01764545 doi (DE-627)OLC2070407853 (DE-He213)BF01764545-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Jossen, J. -A. verfasserin aut A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1992 Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain Filali-Moutei, J. aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 81(1992), 1 vom: Feb., Seite 143-156 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:81 year:1992 number:1 month:02 pages:143-156 https://doi.org/10.1007/BF01764545 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_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 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_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_4193 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4325 GBV_ILN_4337 AR 81 1992 1 02 143-156
allfieldsSound	10.1007/BF01764545 doi (DE-627)OLC2070407853 (DE-He213)BF01764545-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Jossen, J. -A. verfasserin aut A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1992 Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain Filali-Moutei, J. aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 81(1992), 1 vom: Feb., Seite 143-156 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:81 year:1992 number:1 month:02 pages:143-156 https://doi.org/10.1007/BF01764545 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_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 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_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_4193 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4325 GBV_ILN_4337 AR 81 1992 1 02 143-156
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author	Jossen, J. -A.
spellingShingle	Jossen, J. -A. ddc 550 ssgn 13 misc Jurassic misc Evaporite misc Lower Jurassic misc Carbonate Platform misc Atlas Mountain A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains
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topic_title	550 VZ 13 ssgn A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains Jurassic Evaporite Lower Jurassic Carbonate Platform Atlas Mountain
topic	ddc 550 ssgn 13 misc Jurassic misc Evaporite misc Lower Jurassic misc Carbonate Platform misc Atlas Mountain
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title	A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains
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title_full	A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains
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title_sort	a new look at the structural geology of the southern side of the central and eastern high atlas mountains
title_auth	A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains
abstract	Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. © Ferdinand Enke Verlag Stuttgart 1992
abstractGer	Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. © Ferdinand Enke Verlag Stuttgart 1992
abstract_unstemmed	Abstract We give a general description of two evaporite basins discovered, one under, and the other south of the Lower Jurassic carbonate platform which fringes the Atlas Gulf in the south. The larger of these basins lies in the triangle Tazzouguert, Aoufouss, Tarda. The smaller, whose extent is difficult to determine (it being considerably deformed and partially covered over by the southward sliding of the Liassic carbonate platform), lies north of Tinerhir and Ifer. Marl and evaporite Middle Liassic deposits from this smaller basin form a tectonic window in the massive limestones of the Liassic carbonate platform at Tisgui (Todrha gorges). This window clearly shows that the zone in question was affected by southward sliding. To the East of Tazzouguert going towards Bouanane the carbonate platform backs directly onto the African craton. In the area we studied we noticed that the Liassic platform-basin boundary was controlled by at least two major faults (and not just one as we had thought). Between Tinerhir and »Tunnel de la Légion«, the Tizi n'Firest Fault provided the main structural control of sedimentation during the Lias. The open sea is situated North of this fault. East of the oued Ziz valley and 10 kilometers south of »Tunnel de la Légion«, it was the Jbel Dermchane Fault which provided the same control of sedimentation. Finally, we observed a pattern of major faults all along the northern boundary of the Errachidia- Boudenib Cretaceous basin. © Ferdinand Enke Verlag Stuttgart 1992
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title_short	A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains
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A new look at the structural geology of the southern side of the Central and Eastern High Atlas mountains

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