Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)

Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Otmane, Khadija [verfasserIn] Errami, Ezzoura [verfasserIn] Olivier, Philippe [verfasserIn] Berger, Julien [verfasserIn] Triantafyllou, Antoine [verfasserIn] Ennih, Nasser [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco

Übergeordnetes Werk:	Enthalten in: Journal of African earth sciences - Amsterdam [u.a.] : Elsevier Science, 1983, 139, Seite 55-72
Übergeordnetes Werk:	volume:139 ; pages:55-72

DOI / URN:	10.1016/j.jafrearsci.2017.11.030

Katalog-ID:	ELV000840173

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245	1	0	\|a Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
264		1	\|c 2017
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520			\|a Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event.
650		4	\|a Magnetic fabric
650		4	\|a AMS
650		4	\|a Imider dyke swarms
650		4	\|a Eastern Saghro
650		4	\|a Anti-Atlas
650		4	\|a Morocco
700	1		\|a Errami, Ezzoura \|e verfasserin \|4 aut
700	1		\|a Olivier, Philippe \|e verfasserin \|4 aut
700	1		\|a Berger, Julien \|e verfasserin \|4 aut
700	1		\|a Triantafyllou, Antoine \|e verfasserin \|4 aut
700	1		\|a Ennih, Nasser \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Journal of African earth sciences \|d Amsterdam [u.a.] : Elsevier Science, 1983 \|g 139, Seite 55-72 \|h Online-Ressource \|w (DE-627)303391677 \|w (DE-600)1494713-4 \|w (DE-576)096806451 \|x 1879-1956 \|7 nnns
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912			\|a GBV_ILN_370
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912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
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912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
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912			\|a GBV_ILN_2055
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912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
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912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
936	b	k	\|a 38.00 \|j Geowissenschaften: Allgemeines
951			\|a AR
952			\|d 139 \|h 55-72

Indexfelder

author_variant	k o ko e e ee p o po j b jb a t at n e ne
matchkey_str	article:18791956:2017----::antcarcnfodrcinnheicrnmdryewrsatratalsoocifrefote
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publishDate	2017
allfields	10.1016/j.jafrearsci.2017.11.030 doi (DE-627)ELV000840173 (ELSEVIER)S1464-343X(17)30455-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Otmane, Khadija verfasserin aut Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event. Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco Errami, Ezzoura verfasserin aut Olivier, Philippe verfasserin aut Berger, Julien verfasserin aut Triantafyllou, Antoine verfasserin aut Ennih, Nasser verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 139, Seite 55-72 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:139 pages:55-72 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_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2098 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 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 139 55-72
spelling	10.1016/j.jafrearsci.2017.11.030 doi (DE-627)ELV000840173 (ELSEVIER)S1464-343X(17)30455-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Otmane, Khadija verfasserin aut Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event. Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco Errami, Ezzoura verfasserin aut Olivier, Philippe verfasserin aut Berger, Julien verfasserin aut Triantafyllou, Antoine verfasserin aut Ennih, Nasser verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 139, Seite 55-72 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:139 pages:55-72 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_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2098 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 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 139 55-72
allfields_unstemmed	10.1016/j.jafrearsci.2017.11.030 doi (DE-627)ELV000840173 (ELSEVIER)S1464-343X(17)30455-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Otmane, Khadija verfasserin aut Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event. Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco Errami, Ezzoura verfasserin aut Olivier, Philippe verfasserin aut Berger, Julien verfasserin aut Triantafyllou, Antoine verfasserin aut Ennih, Nasser verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 139, Seite 55-72 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:139 pages:55-72 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_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2098 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 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 139 55-72
allfieldsGer	10.1016/j.jafrearsci.2017.11.030 doi (DE-627)ELV000840173 (ELSEVIER)S1464-343X(17)30455-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Otmane, Khadija verfasserin aut Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event. Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco Errami, Ezzoura verfasserin aut Olivier, Philippe verfasserin aut Berger, Julien verfasserin aut Triantafyllou, Antoine verfasserin aut Ennih, Nasser verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 139, Seite 55-72 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:139 pages:55-72 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_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2098 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 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 139 55-72
allfieldsSound	10.1016/j.jafrearsci.2017.11.030 doi (DE-627)ELV000840173 (ELSEVIER)S1464-343X(17)30455-7 DE-627 ger DE-627 rda eng 550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Otmane, Khadija verfasserin aut Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event. Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco Errami, Ezzoura verfasserin aut Olivier, Philippe verfasserin aut Berger, Julien verfasserin aut Triantafyllou, Antoine verfasserin aut Ennih, Nasser verfasserin aut Enthalten in Journal of African earth sciences Amsterdam [u.a.] : Elsevier Science, 1983 139, Seite 55-72 Online-Ressource (DE-627)303391677 (DE-600)1494713-4 (DE-576)096806451 1879-1956 nnns volume:139 pages:55-72 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_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2098 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 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 139 55-72
language	English
source	Enthalten in Journal of African earth sciences 139, Seite 55-72 volume:139 pages:55-72
sourceStr	Enthalten in Journal of African earth sciences 139, Seite 55-72 volume:139 pages:55-72
format_phy_str_mv	Article
bklname	Geowissenschaften: Allgemeines
institution	findex.gbv.de
topic_facet	Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco
dewey-raw	550
isfreeaccess_bool	false
container_title	Journal of African earth sciences
authorswithroles_txt_mv	Otmane, Khadija @@aut@@ Errami, Ezzoura @@aut@@ Olivier, Philippe @@aut@@ Berger, Julien @@aut@@ Triantafyllou, Antoine @@aut@@ Ennih, Nasser @@aut@@
publishDateDaySort_date	2017-01-01T00:00:00Z
hierarchy_top_id	303391677
dewey-sort	3550
id	ELV000840173
language_de	englisch
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author	Otmane, Khadija
spellingShingle	Otmane, Khadija ddc 550 ssgn 6,31 fid AFRIKA bkl 38.00 misc Magnetic fabric misc AMS misc Imider dyke swarms misc Eastern Saghro misc Anti-Atlas misc Morocco Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
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topic_title	550 DE-600 6,31 ssgn AFRIKA DE-30 fid 38.00 bkl Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS) Magnetic fabric AMS Imider dyke swarms Eastern Saghro Anti-Atlas Morocco
topic	ddc 550 ssgn 6,31 fid AFRIKA bkl 38.00 misc Magnetic fabric misc AMS misc Imider dyke swarms misc Eastern Saghro misc Anti-Atlas misc Morocco
topic_unstemmed	ddc 550 ssgn 6,31 fid AFRIKA bkl 38.00 misc Magnetic fabric misc AMS misc Imider dyke swarms misc Eastern Saghro misc Anti-Atlas misc Morocco
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title	Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
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title_full	Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
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author_browse	Otmane, Khadija Errami, Ezzoura Olivier, Philippe Berger, Julien Triantafyllou, Antoine Ennih, Nasser
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title_sort	magnetic fabric and flow direction in the ediacaran imider dyke swarms (eastern anti-atlas, morocco), inferred from the anisotropy of magnetic susceptibility (ams)
title_auth	Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
abstract	Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event.
abstractGer	Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event.
abstract_unstemmed	Located in the Imiter Inlier (Eastern Saghro, Anti-Atlas, Morocco), Ediacaran volcanic dykes have been studied for their petrofabric using Anisotropy of Magnetic Susceptibility (AMS) technique. Four dykes, namely TF, TD, FF and FE show andesitic compositions and are considered to belong to the same dyke swarm. They are oriented respectively N25E, N40E, N50E, and N10E and have been emplaced during a first tectonic event. The dyke FW, oriented N90E displays a composition of alkali basalt and its emplacement is attributed to a subsequent tectonic event.
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title_short	Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)
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author2	Errami, Ezzoura Olivier, Philippe Berger, Julien Triantafyllou, Antoine Ennih, Nasser
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doi_str	10.1016/j.jafrearsci.2017.11.030
up_date	2024-07-06T19:21:30.296Z
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score	7.4019384

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Magnetic fabric and flow direction in the Ediacaran Imider dyke swarms (Eastern Anti-Atlas, Morocco), inferred from the Anisotropy of Magnetic Susceptibility (AMS)

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Vorhandene Bände

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