Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift

Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typic...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Said, Said Mohamed [verfasserIn] Sakran, Shawky [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting

Übergeordnetes Werk:	Enthalten in: Journal of African earth sciences - Amsterdam [u.a.] : Elsevier Science, 1983, 162
Übergeordnetes Werk:	volume:162

DOI / URN:	10.1016/j.jafrearsci.2019.103719

Katalog-ID:	ELV003445488

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allfields	10.1016/j.jafrearsci.2019.103719 doi (DE-627)ELV003445488 (ELSEVIER)S1464-343X(19)30374-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Said, Said Mohamed verfasserin (orcid)0000-0002-6274-9362 aut Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone. Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting Sakran, Shawky verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 162 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:162 GBV_USEFLAG_U SYSFLAG_U GBV_ELV FID-AFRIKA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 162
spelling	10.1016/j.jafrearsci.2019.103719 doi (DE-627)ELV003445488 (ELSEVIER)S1464-343X(19)30374-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Said, Said Mohamed verfasserin (orcid)0000-0002-6274-9362 aut Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone. Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting Sakran, Shawky verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 162 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:162 GBV_USEFLAG_U SYSFLAG_U GBV_ELV FID-AFRIKA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 162
allfields_unstemmed	10.1016/j.jafrearsci.2019.103719 doi (DE-627)ELV003445488 (ELSEVIER)S1464-343X(19)30374-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Said, Said Mohamed verfasserin (orcid)0000-0002-6274-9362 aut Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone. Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting Sakran, Shawky verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 162 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:162 GBV_USEFLAG_U SYSFLAG_U GBV_ELV FID-AFRIKA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 162
allfieldsGer	10.1016/j.jafrearsci.2019.103719 doi (DE-627)ELV003445488 (ELSEVIER)S1464-343X(19)30374-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Said, Said Mohamed verfasserin (orcid)0000-0002-6274-9362 aut Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone. Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting Sakran, Shawky verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 162 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:162 GBV_USEFLAG_U SYSFLAG_U GBV_ELV FID-AFRIKA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 162
allfieldsSound	10.1016/j.jafrearsci.2019.103719 doi (DE-627)ELV003445488 (ELSEVIER)S1464-343X(19)30374-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Said, Said Mohamed verfasserin (orcid)0000-0002-6274-9362 aut Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone. Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting Sakran, Shawky verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 162 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:162 GBV_USEFLAG_U SYSFLAG_U GBV_ELV FID-AFRIKA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 162
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author	Said, Said Mohamed
spellingShingle	Said, Said Mohamed ddc 550 ssgn 6,31 fid AFRIKA bkl 38.00 misc Extensional fault pattern misc Fault-linkage misc Komomombo basin misc Cretaceous rift system misc Multi-phase rifting Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift
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topic_title	550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift Extensional fault pattern Fault-linkage Komomombo basin Cretaceous rift system Multi-phase rifting
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title	Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift
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title_full	Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift
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title_sort	structural analysis and tectonic evolution of the komombo basin, south egypt; an example of interior cretaceous rift
title_auth	Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift
abstract	Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone.
abstractGer	Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone.
abstract_unstemmed	Structural geometry of the Komombo basin was demonstrated using 2D seismic data. Komombo basin appears as two, left-stepping, en-echelon half grabens separated by a NNE oriented broad anticline dissected by NNE oriented oblique-slip faults. The developed fault pattern in the Komombo basin is a typical, non-collinear fault system which encompasses several segments of NW, N–S and WNW orientations. Komombo basin shows along strike variation in the fault pattern. Its southern part is further subdivided into several intrabasinal troughs and highs bounded by synthetic down-dip and antithetic up-dip fault systems, while the northern part is characterized by a synthetic SW dipping step fault pattern producing small eastward rotated half-grabens. The two fault patterns are separated by N–S shear zone.
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title_short	Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift
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doi_str	10.1016/j.jafrearsci.2019.103719
up_date	2024-07-06T19:38:44.359Z
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Structural analysis and tectonic evolution of the Komombo basin, south Egypt; an example of interior Cretaceous rift

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