Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil

The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syeno...
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Autor*in:	Santos, Rodrigo Fabiano Silva [verfasserIn] Oliveira, Davis Carvalho de [verfasserIn] Marangoanha, Bhrenno [verfasserIn] Galarza, Marco Antonio [verfasserIn] Santos, Marcelo Reis [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Granite Paleoproterozoic A-Type Ilmenite series Carajás

Übergeordnetes Werk:	Enthalten in: Lithos - Amsterdam [u.a.] : Elsevier Science, 1968, 462
Übergeordnetes Werk:	volume:462

DOI / URN:	10.1016/j.lithos.2023.107412

Katalog-ID:	ELV065937805

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100	1		\|a Santos, Rodrigo Fabiano Silva \|e verfasserin \|4 aut
245	1	0	\|a Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
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520			\|a The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels.
650		4	\|a Granite
650		4	\|a Paleoproterozoic
650		4	\|a A-Type
650		4	\|a Ilmenite series
650		4	\|a Carajás
700	1		\|a Oliveira, Davis Carvalho de \|e verfasserin \|4 aut
700	1		\|a Marangoanha, Bhrenno \|e verfasserin \|4 aut
700	1		\|a Galarza, Marco Antonio \|e verfasserin \|4 aut
700	1		\|a Santos, Marcelo Reis \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Lithos \|d Amsterdam [u.a.] : Elsevier Science, 1968 \|g 462 \|h Online-Ressource \|w (DE-627)303393181 \|w (DE-600)1494884-9 \|w (DE-576)081952880 \|x 1872-6143 \|7 nnns
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912			\|a GBV_ILN_224
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912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
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_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
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912			\|a GBV_ILN_2021
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912			\|a GBV_ILN_2048
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912			\|a GBV_ILN_2050
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912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2059
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912			\|a GBV_ILN_2088
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912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
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912			\|a GBV_ILN_4333
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936	b	k	\|a 38.25 \|j Petrologie: Allgemeines \|q VZ
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publishDate	2023
allfields	10.1016/j.lithos.2023.107412 doi (DE-627)ELV065937805 (ELSEVIER)S0024-4937(23)00396-1 DE-627 ger DE-627 rda eng 550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Santos, Rodrigo Fabiano Silva verfasserin aut Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels. Granite Paleoproterozoic A-Type Ilmenite series Carajás Oliveira, Davis Carvalho de verfasserin aut Marangoanha, Bhrenno verfasserin aut Galarza, Marco Antonio verfasserin aut Santos, Marcelo Reis verfasserin aut Enthalten in Lithos Amsterdam [u.a.] : Elsevier Science, 1968 462 Online-Ressource (DE-627)303393181 (DE-600)1494884-9 (DE-576)081952880 1872-6143 nnns volume:462 GBV_USEFLAG_U GBV_ELV SYSFLAG_U 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_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_213 GBV_ILN_224 GBV_ILN_230 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_2008 GBV_ILN_2009 GBV_ILN_2010 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_2034 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_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 Petrologie: Allgemeines VZ 38.30 Mineralogie VZ 38.32 Geochemie VZ AR 462
spelling	10.1016/j.lithos.2023.107412 doi (DE-627)ELV065937805 (ELSEVIER)S0024-4937(23)00396-1 DE-627 ger DE-627 rda eng 550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Santos, Rodrigo Fabiano Silva verfasserin aut Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels. Granite Paleoproterozoic A-Type Ilmenite series Carajás Oliveira, Davis Carvalho de verfasserin aut Marangoanha, Bhrenno verfasserin aut Galarza, Marco Antonio verfasserin aut Santos, Marcelo Reis verfasserin aut Enthalten in Lithos Amsterdam [u.a.] : Elsevier Science, 1968 462 Online-Ressource (DE-627)303393181 (DE-600)1494884-9 (DE-576)081952880 1872-6143 nnns volume:462 GBV_USEFLAG_U GBV_ELV SYSFLAG_U 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_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_213 GBV_ILN_224 GBV_ILN_230 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_2008 GBV_ILN_2009 GBV_ILN_2010 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_2034 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_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 Petrologie: Allgemeines VZ 38.30 Mineralogie VZ 38.32 Geochemie VZ AR 462
allfields_unstemmed	10.1016/j.lithos.2023.107412 doi (DE-627)ELV065937805 (ELSEVIER)S0024-4937(23)00396-1 DE-627 ger DE-627 rda eng 550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Santos, Rodrigo Fabiano Silva verfasserin aut Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels. Granite Paleoproterozoic A-Type Ilmenite series Carajás Oliveira, Davis Carvalho de verfasserin aut Marangoanha, Bhrenno verfasserin aut Galarza, Marco Antonio verfasserin aut Santos, Marcelo Reis verfasserin aut Enthalten in Lithos Amsterdam [u.a.] : Elsevier Science, 1968 462 Online-Ressource (DE-627)303393181 (DE-600)1494884-9 (DE-576)081952880 1872-6143 nnns volume:462 GBV_USEFLAG_U GBV_ELV SYSFLAG_U 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_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_213 GBV_ILN_224 GBV_ILN_230 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_2008 GBV_ILN_2009 GBV_ILN_2010 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_2034 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_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 Petrologie: Allgemeines VZ 38.30 Mineralogie VZ 38.32 Geochemie VZ AR 462
allfieldsGer	10.1016/j.lithos.2023.107412 doi (DE-627)ELV065937805 (ELSEVIER)S0024-4937(23)00396-1 DE-627 ger DE-627 rda eng 550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Santos, Rodrigo Fabiano Silva verfasserin aut Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels. Granite Paleoproterozoic A-Type Ilmenite series Carajás Oliveira, Davis Carvalho de verfasserin aut Marangoanha, Bhrenno verfasserin aut Galarza, Marco Antonio verfasserin aut Santos, Marcelo Reis verfasserin aut Enthalten in Lithos Amsterdam [u.a.] : Elsevier Science, 1968 462 Online-Ressource (DE-627)303393181 (DE-600)1494884-9 (DE-576)081952880 1872-6143 nnns volume:462 GBV_USEFLAG_U GBV_ELV SYSFLAG_U 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_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_213 GBV_ILN_224 GBV_ILN_230 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_2008 GBV_ILN_2009 GBV_ILN_2010 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_2034 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_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 Petrologie: Allgemeines VZ 38.30 Mineralogie VZ 38.32 Geochemie VZ AR 462
allfieldsSound	10.1016/j.lithos.2023.107412 doi (DE-627)ELV065937805 (ELSEVIER)S0024-4937(23)00396-1 DE-627 ger DE-627 rda eng 550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Santos, Rodrigo Fabiano Silva verfasserin aut Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels. Granite Paleoproterozoic A-Type Ilmenite series Carajás Oliveira, Davis Carvalho de verfasserin aut Marangoanha, Bhrenno verfasserin aut Galarza, Marco Antonio verfasserin aut Santos, Marcelo Reis verfasserin aut Enthalten in Lithos Amsterdam [u.a.] : Elsevier Science, 1968 462 Online-Ressource (DE-627)303393181 (DE-600)1494884-9 (DE-576)081952880 1872-6143 nnns volume:462 GBV_USEFLAG_U GBV_ELV SYSFLAG_U 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_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_213 GBV_ILN_224 GBV_ILN_230 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_2008 GBV_ILN_2009 GBV_ILN_2010 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_2034 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_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 Petrologie: Allgemeines VZ 38.30 Mineralogie VZ 38.32 Geochemie VZ AR 462
language	English
source	Enthalten in Lithos 462 volume:462
sourceStr	Enthalten in Lithos 462 volume:462
format_phy_str_mv	Article
bklname	Petrologie: Allgemeines Mineralogie Geochemie
institution	findex.gbv.de
topic_facet	Granite Paleoproterozoic A-Type Ilmenite series Carajás
dewey-raw	550
isfreeaccess_bool	false
container_title	Lithos
authorswithroles_txt_mv	Santos, Rodrigo Fabiano Silva @@aut@@ Oliveira, Davis Carvalho de @@aut@@ Marangoanha, Bhrenno @@aut@@ Galarza, Marco Antonio @@aut@@ Santos, Marcelo Reis @@aut@@
publishDateDaySort_date	2023-01-01T00:00:00Z
hierarchy_top_id	303393181
dewey-sort	3550
id	ELV065937805
language_de	englisch
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author	Santos, Rodrigo Fabiano Silva
spellingShingle	Santos, Rodrigo Fabiano Silva ddc 550 bkl 38.25 bkl 38.30 bkl 38.32 misc Granite misc Paleoproterozoic misc A-Type misc Ilmenite series misc Carajás Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
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topic_title	550 VZ 38.25 bkl 38.30 bkl 38.32 bkl Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil Granite Paleoproterozoic A-Type Ilmenite series Carajás
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title	Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
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title_full	Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
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author_browse	Santos, Rodrigo Fabiano Silva Oliveira, Davis Carvalho de Marangoanha, Bhrenno Galarza, Marco Antonio Santos, Marcelo Reis
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title_sort	geochemistry, zircon u-pb geochronology and lu-hf isotopes of the manda saia granite: petrological affinity and magma source of evolved a-type granites from the carajás province, southeastern amazonian craton, brazil
title_auth	Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
abstract	The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels.
abstractGer	The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels.
abstract_unstemmed	The Manda Saia granite occurs in the Carajás province, southeastern Amazonian craton, and it is represented by two semicircular intrusive stocks in the Mesoarchean granitoid and greenstone belt sequence of the Rio Maria domain. The stocks are composed of hololeucocratic, red-colored monzo- and syenogranite rocks. Biotite is the main ferromagnesian mineral, and amphibole is rare and was formed later. The rocks are ferroan, calk-alkalic, peraluminous and present a restricted and high SiO2 range (74.80 and 77.70%), high FeOt/FeOt+MgO (0.89–0.98) ratios and enrichment in rare earth elements (REEs, 111–497 ppm), with moderate negative Eu anomalies (0.04–0.63). The plutons are classified as ferroan A-type granites and were formed under moderately reduced to moderately oxidized conditions, similar to those those in the Serra dos Carajás suite. They also show affinities with the more evolved members from both the reduced Velho Guilherme suite and oxidized Jamon suite from the Carajás province. The Manda Saia granite has a zircon U-Pb crystallization age of 1866 ± 10 Ma and is derived from partial melting of the Mesoarchean crust of tonalitic composition, as indicated by strongly negative ƐHf values (−12 to −18). The emplacement of these plutons is related to extensional tectonics with magma transport at shallow crustal levels.
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title_short	Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil
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doi_str	10.1016/j.lithos.2023.107412
up_date	2024-07-07T00:46:02.751Z
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Geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of the Manda Saia granite: Petrological affinity and magma source of evolved A-type granites from the Carajás province, southeastern Amazonian craton, Brazil

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