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...
Ausführliche Beschreibung
Autor*in: |
Santos, Rodrigo Fabiano Silva [verfasserIn] Oliveira, Davis Carvalho de [verfasserIn] Marangoanha, Bhrenno [verfasserIn] Galarza, Marco Antonio [verfasserIn] Santos, Marcelo Reis [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2023 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Lithos - Amsterdam [u.a.] : Elsevier Science, 1968, 462 |
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Übergeordnetes Werk: |
volume:462 |
DOI / URN: |
10.1016/j.lithos.2023.107412 |
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Katalog-ID: |
ELV065937805 |
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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. | ||
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700 | 1 | |a Galarza, Marco Antonio |e verfasserin |4 aut | |
700 | 1 | |a Santos, Marcelo Reis |e verfasserin |4 aut | |
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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 |
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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 |
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Enthalten in Lithos 462 volume:462 |
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Granite Paleoproterozoic A-Type Ilmenite series Carajás |
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Santos, Rodrigo Fabiano Silva @@aut@@ Oliveira, Davis Carvalho de @@aut@@ Marangoanha, Bhrenno @@aut@@ Galarza, Marco Antonio @@aut@@ Santos, Marcelo Reis @@aut@@ |
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2023-01-01T00:00:00Z |
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Santos, Rodrigo Fabiano Silva |
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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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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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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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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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Santos, Rodrigo Fabiano Silva Oliveira, Davis Carvalho de Marangoanha, Bhrenno Galarza, Marco Antonio Santos, Marcelo Reis |
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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 |
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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