The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)

The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consis...
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Autor*in:	Barbero, Edoardo [verfasserIn] Delavari, Morteza [verfasserIn] Dolati, Asghar [verfasserIn] Saccani, Emilio [verfasserIn] Marroni, Michele [verfasserIn] Catanzariti, Rita [verfasserIn] Pandolfi, Luca [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous

Übergeordnetes Werk:	Enthalten in: Journal of Asian earth sciences - Amsterdam [u.a.] : Elsevier Science, 1997, 195
Übergeordnetes Werk:	volume:195

DOI / URN:	10.1016/j.jseaes.2020.104306

Katalog-ID:	ELV004132920

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520			\|a The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks.
650		4	\|a Volcanic arc
650		4	\|a Geochemistry
650		4	\|a Stratigraphy
650		4	\|a Makran
650		4	\|a Iran
650		4	\|a Late Cretaceous
700	1		\|a Delavari, Morteza \|e verfasserin \|4 aut
700	1		\|a Dolati, Asghar \|e verfasserin \|4 aut
700	1		\|a Saccani, Emilio \|e verfasserin \|0 (orcid)0000-0001-9879-2795 \|4 aut
700	1		\|a Marroni, Michele \|e verfasserin \|4 aut
700	1		\|a Catanzariti, Rita \|e verfasserin \|4 aut
700	1		\|a Pandolfi, Luca \|e verfasserin \|0 (orcid)0000-0002-6129-647X \|4 aut
773	0	8	\|i Enthalten in \|t Journal of Asian earth sciences \|d Amsterdam [u.a.] : Elsevier Science, 1997 \|g 195 \|h Online-Ressource \|w (DE-627)303391960 \|w (DE-600)1494743-2 \|w (DE-576)106846035 \|x 1878-5786 \|7 nnns
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936	b	k	\|a 38.00 \|j Geowissenschaften: Allgemeines
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author_variant	e b eb m d md a d ad e s es m m mm r c rc l p lp
matchkey_str	article:18785786:2020----::hgncmlxenepeeaaaertcosocncripiainfrhgoyaieouin
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publishDate	2020
allfields	10.1016/j.jseaes.2020.104306 doi (DE-627)ELV004132920 (ELSEVIER)S1367-9120(20)30087-0 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Barbero, Edoardo verfasserin (orcid)0000-0003-0247-0770 aut The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks. Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous Delavari, Morteza verfasserin aut Dolati, Asghar verfasserin aut Saccani, Emilio verfasserin (orcid)0000-0001-9879-2795 aut Marroni, Michele verfasserin aut Catanzariti, Rita verfasserin aut Pandolfi, Luca verfasserin (orcid)0000-0002-6129-647X aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 195 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV 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_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 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 195
spelling	10.1016/j.jseaes.2020.104306 doi (DE-627)ELV004132920 (ELSEVIER)S1367-9120(20)30087-0 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Barbero, Edoardo verfasserin (orcid)0000-0003-0247-0770 aut The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks. Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous Delavari, Morteza verfasserin aut Dolati, Asghar verfasserin aut Saccani, Emilio verfasserin (orcid)0000-0001-9879-2795 aut Marroni, Michele verfasserin aut Catanzariti, Rita verfasserin aut Pandolfi, Luca verfasserin (orcid)0000-0002-6129-647X aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 195 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV 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_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 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 195
allfields_unstemmed	10.1016/j.jseaes.2020.104306 doi (DE-627)ELV004132920 (ELSEVIER)S1367-9120(20)30087-0 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Barbero, Edoardo verfasserin (orcid)0000-0003-0247-0770 aut The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks. Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous Delavari, Morteza verfasserin aut Dolati, Asghar verfasserin aut Saccani, Emilio verfasserin (orcid)0000-0001-9879-2795 aut Marroni, Michele verfasserin aut Catanzariti, Rita verfasserin aut Pandolfi, Luca verfasserin (orcid)0000-0002-6129-647X aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 195 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV 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_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 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 195
allfieldsGer	10.1016/j.jseaes.2020.104306 doi (DE-627)ELV004132920 (ELSEVIER)S1367-9120(20)30087-0 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Barbero, Edoardo verfasserin (orcid)0000-0003-0247-0770 aut The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks. Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous Delavari, Morteza verfasserin aut Dolati, Asghar verfasserin aut Saccani, Emilio verfasserin (orcid)0000-0001-9879-2795 aut Marroni, Michele verfasserin aut Catanzariti, Rita verfasserin aut Pandolfi, Luca verfasserin (orcid)0000-0002-6129-647X aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 195 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV 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_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 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 195
allfieldsSound	10.1016/j.jseaes.2020.104306 doi (DE-627)ELV004132920 (ELSEVIER)S1367-9120(20)30087-0 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Barbero, Edoardo verfasserin (orcid)0000-0003-0247-0770 aut The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks. Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous Delavari, Morteza verfasserin aut Dolati, Asghar verfasserin aut Saccani, Emilio verfasserin (orcid)0000-0001-9879-2795 aut Marroni, Michele verfasserin aut Catanzariti, Rita verfasserin aut Pandolfi, Luca verfasserin (orcid)0000-0002-6129-647X aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 195 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV 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_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 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 195
language	English
source	Enthalten in Journal of Asian earth sciences 195 volume:195
sourceStr	Enthalten in Journal of Asian earth sciences 195 volume:195
format_phy_str_mv	Article
bklname	Geowissenschaften: Allgemeines
institution	findex.gbv.de
topic_facet	Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous
dewey-raw	550
isfreeaccess_bool	false
container_title	Journal of Asian earth sciences
authorswithroles_txt_mv	Barbero, Edoardo @@aut@@ Delavari, Morteza @@aut@@ Dolati, Asghar @@aut@@ Saccani, Emilio @@aut@@ Marroni, Michele @@aut@@ Catanzariti, Rita @@aut@@ Pandolfi, Luca @@aut@@
publishDateDaySort_date	2020-01-01T00:00:00Z
hierarchy_top_id	303391960
dewey-sort	3550
id	ELV004132920
language_de	englisch
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author	Barbero, Edoardo
spellingShingle	Barbero, Edoardo ddc 550 bkl 38.00 misc Volcanic arc misc Geochemistry misc Stratigraphy misc Makran misc Iran misc Late Cretaceous The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)
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topic_title	550 DE-600 38.00 bkl The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran) Volcanic arc Geochemistry Stratigraphy Makran Iran Late Cretaceous
topic	ddc 550 bkl 38.00 misc Volcanic arc misc Geochemistry misc Stratigraphy misc Makran misc Iran misc Late Cretaceous
topic_unstemmed	ddc 550 bkl 38.00 misc Volcanic arc misc Geochemistry misc Stratigraphy misc Makran misc Iran misc Late Cretaceous
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title	The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)
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title_full	The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)
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title_sort	the ganj complex reinterpreted as a late cretaceous volcanic arc: implications for the geodynamic evolution of the north makran domain (southeast iran)
title_auth	The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)
abstract	The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks.
abstractGer	The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks.
abstract_unstemmed	The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is represented by a >2000 m thick sequence consisting of a dyke-swarm showing transition to a volcano-sedimentary sequence with local interlayerings of turbidite beds. This sequence grades-up to a turbidite sequence whose calcareous nannofossil biostratigraphy indicates a Turonian-Coniacian age. Volcanic rocks and dykes are represented mainly by intermediate and acidic rocks and minor basalts. They show volcanic arc affinity, with calc-alkaline and island arc tholeiitic compositions, which locally show adakite signature. In the turbiditic arenites, volcanic-derived debris is predominant and it is associated with moderate amounts of coheval calcareous rock fragments and bioclasts; thus suggesting sediment provenance from intrabasinal volcanic arc and carbonatic platform source rocks.
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title_short	The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)
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The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)

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