Petrologia do Stock Serra da Vaca, Domínio Poço Redondo, Sistema Orogênico Sergipano

Douglas Barreto de  Oliveira; Herbet  Conceição; Maria de Lourdes da Silva  Rosa

doi:10.11606/issn.2316-9095.v21-163165

Authors

Douglas Barreto de Oliveira Universidade Federal de Sergipe. https://orcid.org/0000-0003-0338-1155
Herbet Conceição Universidade Federal de Sergipe. https://orcid.org/0000-0002-9172-4519
Maria de Lourdes da Silva Rosa Universidade Federal de Sergipe. https://orcid.org/0000-0002-5099-829X

DOI:

https://doi.org/10.11606/issn.2316-9095.v21-163165

Keywords:

Serra da Vaca Stock, Orogenic Granite, Sergipe, Borborema Province

Abstract

Serra da Vaca Stock (SSV, 19 km2) is elongated NE-SW, located in the North of Poço Redondo Domain, in the Sergipano
Orogenic System. The orientation of this stock cut off the NW-SE regional metamorphic foliation. SVS is composed of biotite
gray leucocratic granodiorites of gray color, fine to medium equigranular texture, of isotropic structure. Syenogranites and
alkali-feldspar granite are present. The accessory minerals of these rocks are epidote, zircon, apatite, and opaque minerals.
Alkaline feldspar is perthitic. Andesine and oligoclase of granodiorites have normal zonation, indicating fractional crystallization. Brown biotite is primary and has Fe/(Fe+Mg) ratio ranging from 0.47–0.84 and exhibits chemical affinity for calcalkaline suites. The primary epidote (19.9 < %pistacite < 28.85) indicates crystallization under relatively oxidizing conditions at a pressure of 6 kbar (~25 km). Geochemical data indicate that SVS rocks are evolved (70% < SiO2 < 77.5%), peraluminous and magnesian. The magmatic affiliation of granodiorites is high K calc-alkaline, whereas syenogranites, which are the most evolved, have shoshonitic affinity. The (La/Yb)N ratios range from 21–70 of granodiorites, 40 in the alkali granite, and 1.4–2.8 in the sienogranites. Eu anomalies are poorly pronounced for most samples (0.57 < Eu/Eu* < 0.94), except for alkali-granite and syenogranites, which exhibit a strong europium negative anomaly (0.16–0.3). Data on trace elements suggest that SVS magma was formed from potassium mafic igneous protoliths. Relations between trace elements (e.g., Th, Ta, Hf, Y, Nb, Rb) indicate that these granites were generated in an orogenic environment in a post-tectonic period. SSV granodiorites are suggested to belong to the Coronel João Sá Intrusive Suite of the Macururé Domain, since they have a geochemical signature

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References

Almeida, F. F. M., Brito Neves, B. B., Fuck, R. A. (1977). Províncias Estruturais Brasileiras. In: VIII Simpósio Geologia do Nordeste. Atas..., p. 363-391. Campina Grande: SBG.

Barbarin, B. (1999). A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos, 46(3), 605-626. https://doi.org/10.1016/S0024-4937(98)00085-1

Bowden, P., Batchelor, R. A., Chappell, B. W., Didier, J., Lameyre, J. (1984). Petrological, geochemical and source criteria for the classification of granitic rocks: a discussion. Physics of the Earth and Planetary Interiors, 35(1-3), 1-11. https://doi.org/10.1016/0031-9201(84)90029-3

Brandon, A. D., Creaser, R. A., Chacko, T. (1996). Constraints on rates of granitic magma transport from epidote dissolution kinetics. Science, 271(5257), 1845-1848. https://doi.org/10.1126/Science.271.5257.1845

Brasilino, R. G., Sial, A. N., Ferreira, V. P., Pimentel, M. M. (2011). Bulk rock and mineral chemistries and ascent rates of high-K calc-alkalic epidote-bearing magmas, Northeastern Brazil. Lithos, 127(3-4), 441-454. https://doi.org/10.1016/j.lithos.2011.09.017

Brito Neves, B. B., Sial, A. N., Albuquerque, J. P. T. (1977). Vergência centrífuga residual no sistema de dobramentos Sergipano. Revista Brasileira de Geociências, 7(2), 102-114.

Bueno, J. F., Oliveira, E. P., McNaughton, N., Laux, J. H. (2009). U–Pb dating of granites in the Neoproterozoic Sergipano Belt, NE-Brazil: Implications for the timing and duration of continental collision and extrusion tectonics in the Borborema Province. Gondwana Research, 15(1), 86-97. https://doi.org/10.1016/j.gr.2008.06.003

Carvalho, M. J. (2005). Evolução Tectônica do Domínio Marancó – Poço Redondo: Registro das Orogêneses Cariris Velhos e Brasiliana na Faixa Sergipana, NE do Brasil. Tese (Doutorado). Campinas: Universidade Estadual de Campinas.

Chappell, B. W., White, A. J. R. (1992). I- and S-type granites in the Lachlan Fold Belt. Transaction of Royal Society Edinburg: Earth Sciences, 83(1-2), 1-26. https://doi.org/10.1017/S0263593300007720

Chappell, B. W., White, A. J. R. (2001). Two contrasting granite types: 25 years later. Australian Journal of Earth Sciences, 48(4), 489-499. https://doi.org/10.1046/j.1440-0952.2001.00882.x

Conceição, H., Rosa, M. L. S., Conceição, J. A., Lisboa, V. A. C., Pereira, F. S., Teles, D. S., Fernandes, D. M., Sousa, E. S., Cruz, J. W. S., Rezende, H. J. C., Oliveira, I. R., Souza, J. M. D. S., Oliveira, I. L. (2017). Magmatismos no Domínio Macururé, Sistema Orogênico Sergipano: estado de conhecimento. XXVII Simpósio de Geologia do Nordeste. João Pessoa: SBG.

Conceição, J. A., Rosa, M. L. S., Conceição, H. (2016). Sienogranitos leucocráticos do Domínio Macururé, Sistema Orogênico Sergipano, Nordeste do Brasil: Stock Glória Sul. Brazilian Journal of Geology, 46(1), 63-77. https://doi.org/10.1590/2317-4889201620150044

Corriveau, L., Gorton, M. P. (1993). Coexisting K-rich alkaline and shoshonitic magmatism arc affinities in the Proterozoic: a reassessment of syenitic stocks in the southwestern Grenville Province. Contribution to Mineralogy and Petrology, 113, 262-279. https://doi.org/10.1007/BF00283233

Davison, I., Santos, R. A. (1989). Tectonic evolution of the Sergipano fold belt, NE Brazil, during the Brasiliano orogeny. Precambrian Research, 45(4), 319-342. https://doi.org/10.1016/0301-9268(89)90068-5

Deer, W. A., Howie, R. A., Zussman, J. (1992). An Introduction to the Rock-Forming Mineral. 2. ed. Harlow: Longman Scientific and Technical.

Ferreira, V. P., Sial, A. N., Pimentel, M. M., Armstrong, R., Spicuzza, M., Guimarães, I. P., Silva Filho, A. F. (2011). Contrasting sources and P-T crystallization conditions of epidote-bearing granitic rocks, northeastern Brazil: O, Sr, and Nd Isotopes. Lithos, 121(1-4), 189-201. https://doi.org/10.1016/j.lithos.2010.11.002

Fowler, M. B., Kocks, H., Darbyshire, D. P. F., Greenwood, P. B. (2008). Petrogenesis of high Ba-Sr plutons from the Northern Highlands Terrane of the British Caledonian Province. Lithos, 105(1-2), 129-148. https://doi.org/10.1016/j.lithos.2008.03.003

Frost, R. B. (1991). Introduction to oxigen fugacity and its petrologic importance. In: D. H. Lindsley (Ed.). Oxide minerals: petrologic and magnetic significance (v. 25, p. 1-10). Reviews in Mineralogy. Mineralogical Society of America.

Frost, B. R., Barnes, C. G., Collins, W. J., Arculus, R. J., Ellis, D. J., Frost, C. D. (2001). A geochemical classification of granitic rocks. Journal of Petrology, 42(11), 2033-2048. https://doi.org/10.1093/petrology/42.11.2033

Fuhrman, M. L., Lindsley, D. H. (1988). Ternary-feldspar modeling and thermometry. American Mineralogist, 73(3-4), 201-215.

Galindo, A. C., Silva, F. C. A., Souza, Z. S. (2012). Química mineral de leucomicrogranitos neoproterozoicos do Domínio Rio Grande do Norte. Geochimica Brasiliensis, 26(1), 19-28.

Gorton, M. P., Schandl, E. S. (2000). From Continents to Island Arc: A Geochemical Index of Tectonic Setting for Arc-Related and within Plate Felsic to Intermediate Volcanic Rocks. Canadian Mineralogist, 38(5), 1065-1073. https://doi.org/10.2113/gscanmin.38.5.1065

Gouveia, S. G. (2016). Contribuição à petrografia e geoquímica do Stock Umbuzeiro do Matuto, Sistema Orogênico Sergipano. Trabalho de Conclusão de Curso. São Cristóvão: Universidade Federal de Sergipe – UFS.

Hanson, G. N. (1980). Rare earth elements in petrogenetic studies of igneous systems. Annual Review of Earth and Planetary Sciences, 8, 371-405. https://doi.org/10.1146/annurev.ea.08.050180.002103

Humphrey, L., Allard, G. O. (1967). O Geossinclinal de Propriá – província tectônica do pré-cambriano posterior, recém descoberta no escudo brasileiro. Boletim Técnico da Petrobras, 10(3-4), 409-430.

Johnston, A. D., Wyllie, P. J. (1988). Constraints on the origin of Archeant trondhjejemites based on phase relationships of Nuk gneiss with H2O at 15 kbar. Contributions to Mineralogy and Petrology, 100, 35-46. https://doi.org/10.1007/BF00399438

Lameyre, J., Bowden, P. (1982). Plutonic rocks types series: discrimination of various granitoide series and related rocks. Volcanology and Geothermal Research, 14(1-2), 169-186. https://doi.org/10.1016/0377-0273(82)90047-6

Laurent, O., Martin, H., Moyen, J. F., Doucelance, R. (2014). The diversity and evolution of late-Archean granitoids: Evidence for the onset of “modern-style” plate tectonics between 3.0 and 2.5 Ga. Lithos, 205, 208-235. https://doi.org/10.1016/j.lithos.2014.06.012

Le Maitre, R. W., Streckeisen, A., Zanettin, B., Le Bas, M. J., Bonin, B., Bateman, P., Bellieni, G., Dudek, A., Efremova, S., Keller, J., Lameyre, J., Sabine, P. A., Schimd, R., Sorensen, H., Woolley, A. R. (2002). Igneous Rocks – A classification and glossary of terms. Recommendations of the International Union of Geological Sciences-Subcommission on the Systematics of Igneous Rocks. 2. ed. Nova York: Cambridge University Press.

Lima, D. R. (2016). Caracterização petrológica e geoquímica do Plúton Curituba, Domínio Poço Redondo-Marancó, Cinturão Sergipano. Dissertação (Mestrado). Recife: Universidade Federal de Pernambuco.

Lima, M. M. C. (2013). Caracterização geoquímica, isotópica e geotectônica dos Complexos Araticum e Arapiraca, Faixa Sergipana, Alagoas, Nordeste do Brasil. Dissertação (Mestrado). Recife: Universidade Federal de Pernambuco.

Lisboa, V. A. C., Conceição, H., Rosa, M. L. S., Fernandes, D. M. (2019). The onset of post-collisional magmatism in the Macururé Domain, Sergipano Orogenic System: the Glória Norte Stock. Journal of South American Earth Sciences, 89, 173-188. https://doi.org/10.1016/j.jsames.2018.11.005

Long, L. E., Castellana, C. H., Sial, A. N. (2005). Age, origin and cooling history of the Coronel João Sá Pluton, Bahia, Brazil. Journal of Petrology, 46(2), 255-273. https://doi.org/10.1093/petrology/egh070

Loomis, T. P. (1982). Numerical simulations of cristallization processes of plagioclase in complex melts: the origin of major and Oscillatory zoning in plagioclase. Contributions to Mineralogy and Petrology, 81, 219-229. https://doi.org/10.1007/BF00371299

Maniar, P. D., Piccoli, P. M. (1989). Tectonic discrimination of granitoids. Geological Society American, 101(5), 635-643. https://doi.org/10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2

Mendes, V. A., Brito, M. F. L., Santos, C. A. (2011). Zona de cisalhamento contracional de Palmeira dos Índios. Um possível testemunho do evento Cariris Velhos na Província Borborema. In: XIII Simpósio Nacional de Estudos Tectônicos. Resumo expandido. Campinas.

Middlemost, E. A. K. (1985). Magmas and Magmatic Rocks: an Introduction to Igneous Petrology. Londres e Nova York: Longman, p. 253-257.

Nachit, H., Ibhi, A., Abia, E. H., Ohoud, M. B. (2005). Discrimination between primary magmatic biotites, reequilibrated and neoformed biotites. Comptes Rendus Geoscience, 337(16), 1415-1420. https://doi.org/10.1016/j.crte.2005.09.002

Nachit, H., Razafimahefa, N., Stussi, J. M., Carron, J. P. (1985). Composition chimiquedes biotites et typologie magmatiquedes granitoides. Comptes Rendus deI’Académie des Sciences Paris, 301, 813-818.

Nakamura, N. (1974). Determination of RRE, Ba, Fe, Mg, Na and K in carbonaceus and ordinary chondrites. Geochimica et Cosmochimica Acta, 38(5), 757-775. https://doi.org/10.1016/0016-7037(74)90149-5

Naney, M. T. (1983). Phase equilibria of rock-forming ferromagnesian silicates in granitic systems. American Journal of Sciences, 283(10), 993-1033. https://doi.org/10.2475/ajs.283.10.993

Neves, S. P., Silva, J. M. R., Bruguier, O. (2016). The transition zone between the Pernambuco-Alagoas Domain and the Sergipano belt (Borborema Province, NE Brasil): Geochronological constraints on the ages of deposition, tectonic setting and metamorphism of metasedimentary rocks. Journal of South American Earth Sciences, 72, 266-278. https://doi.org/10.1016/j.jsames.2016.09.010

Oliveira, D. B. (2016). Aspectos Geológicos, Petrográficos e Geoquímicos do Stock Serra da Vaca, Sistema Orogênico Sergipano. Trabalho de Conclusão de Curso. São Cristóvão: Universidade Federal de Sergipe.

Oliveira, E. P., Bueno, J. F., McNaughton, N. J., Silva Filho, A. F., Nascimento, R. S., Donatti-Filho, J. P. (2015). Age, composition, and source of continental arc- and syn-collision granites of the Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil. Journal of South American Earth Sciences, 58, 257-280. https://doi.org/10.1016/j.jsames.2014.08.003

Oliveira, E. P., Windley, B. F., Araújo, M. N. C. (2010). The Neoproterozoic Sergipano orogenic belt, NE Brazil: a complete plate tectonic cycle in western Gondwana. Precambrian Research, 181(1-4), 64-84. https://doi.org/10.1016/j.precamres.2010.05.014

Oliveira, E. P., Windley, B. F., McNaughton, N. J., Bueno, J. F., Nascimento, R. S., Carvalho, M. J., Araújo, M. N. C. (2017). The Sergipano Belt. In: M. Heilbron, U. Cordani, F. Alkmim (Eds.), São Francisco Craton, Eastern Brazil. Regional Geology Reviews. Cham: Springer. https://doi.org/10.1007/978-3-319-01715-0_13

Pearce, J. A. (1996). Source and settings of Granites rocks. Episodes, 19(4), 120-125. https://doi.org/10.18814/epiiugs/1996/v19i4/005

Pearce, J. A., Harris, N. B. W., Tindle, A. G. (1984). Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, 25(4), 956-983. https://doi.org/10.1093/petrology/25.4.956

Peccerillo, A., Taylor, S. R. (1976). Geochemistry of Eocene Calc-Alkaline Volcanic Rocks form the Kastamonu Area, Northen Turkey. Contribution Mineralogy Petrology, 58, 63-81. https://doi.org/10.1007/BF00384745

Pinho Neto, M. A., Rosa, M. L. S., Conceição, H. (2019). Petrologia do Batólito Sítios Novos, Sistema Orogênico Sergipano, Província Borborema, NE do Brasil. Geologia USP. Série Científica, 19(2), 135-150. https://doi.org/10.11606/issn.2316-9095.v19-152469

Santos, I. S., Conceição, H., Rosa, M. L. S., Marinho, M. M. (2019). Magmatismos shoshonítico e cálcio-alcalino de alto potássio (615 Ma) na porção leste do Domínio Macururé, Sistema Orogênico Sergipano: Stocks Propriá, Amparo do São Francisco e Fazenda Alvorada. Geologia USP. Série Científica, 19(1), 99-116. https://doi.org/10.11606/issn.2316-9095.v19-141362

Santos, R. A., Martins, A. A. M., Neves, J. P., Leal, R. A. (1998). Programa de Levantamentos Geológicos Básicos do Brasil: Geologia e Recursos Minerais do Estado de Sergipe. Escala 1:250.000. Texto explicativo do mapa geológico do Estado de Sergipe. Salvador: CPRM/DIEDIG/DEPAT; CODISE.

Santos, R. A., Menezes Filho, N. R., Souza, J. D. (1988). Programa de Levantamentos Geológicos Básicos do Brasil: carta geológica, carta metalogenética/previsional – Escala 1:100.00 (Folha SC.24-X-C-VI Piranhas). Sergipe, Alagoas e Bahia: DNPM/CPRM, 154 p.

Schmidt, M. W., Thompson, A. B. (1996). Epidote in calcalkaline magmas: an experimental study of stability, phase relationships, and the role of epidote in Magmatic evolution. American Mineralogist, 81(3-4), 462-474. https://doi.org/10.2138/am-1996-3-420

Sial, A. N. (1990). Epidote-bearing calc-alkaline granitoids in Northeast Brazil. Revista Brasileira de Geociências, 20(1-4), 88-100.

Sial, A. N., Ferreira, V. P. (2016). Magma associations in Ediacaran granitoids of the Cachoeirinha-Salgueiro and Alto Pajéu terrane, northeastern Brazil: Forty years of studies. Journal of South American Earth Sciences, 68, 113-133. https://doi.org/10.1016/j.jsames.2015.10.005

Silva Filho, M. A., Bomfim, L. F. C., Santos, R. A., Leal, R. A., Santana, A. C., Filho, P. A. B. (1979). Geologia da Geossinclinal Sergipana e do seu embasamento - Alagoas, Sergipe e Bahia: Projeto Baixo São Francisco/Vaza-Barris. Brasília: DNPM/CPRM.

Soares, H. S., Sousa, C. S., Conceição, H., Rosa, M. L. S. (2018). Caracterização Geológica, Petrográfica e Geoquímica dos Stocks Santa Maria e Monte Pedral, Domínio Canindé, Sistema Orogênico Sergipano. Scientia Plena, 14(1), 1-12. https://doi.org/10.14808/sci.plena.2018.015301

Soares, H. S., Sousa, C. S., Rosa, M. L. S., Conceição, H. (2019). Petrologia dos Stocks Santa Maria, Monte Pedral, Bom Jardim, Boa Esperança e Niterói, Suíte Intrusiva Serra do Catu, Estado de Sergipe, NE Brasil. Geologia USP. Série Científica, 19(4), 63-84. https://doi.org/10.11606/issn.2316-9095.v19-156598

Sousa, C. S., Soares, H. S., Rosa, M. L. S, Conceição, H. (2019). Petrologia e geocronologia do Batólito Rio Jacaré, Domínio Poço Redondo, Sistema Orogênico Sergipano, NE do Brasil. Geologia USP. Série Científica, 19(2), 171-194. https://doi.org/10.11606/issn.2316-9095.v19-152494

Speer, J. A. (1984). Micas in igneous rocks. In: S. W. Bailey (ed.). Reviews in Mineralogy (v. 13, p. 299-356). Blacksburg: Mineralogical Society of America. https://doi.org/10.1515/9781501508820-013

Streckeisen, A. L. (1976). To each plutonic rock its proper name. Earth Science Reviews, 12(1), 1-33. https://doi.org/10.1016/0012-8252(76)90052-0

Sylvester, P. J. (1989). Post-collisional alkaline granites. Journal of Geology, 97(3), 261-280. Disponível em: https://www.jstor.org/stable/30068745. Acesso em: 7 maio 2021.

Teixeira, L. R., Lima, E. S., Neves, J. P., Santos, R. A., Santiago, R. C., Melo, R. C. (2014). Mapa Geológico e de Recursos Minerais do Estado de Sergipe. Escala 1:250.000. Aracaju: CPRM-CODISE.

Thompson, R. N. (1982). Magmatism of the British Tertiary volcanic Province. Scottish Journal of Geology, 18, 49-107. https://doi.org/10.1144/sjg18010049

Tulloch, A. J. (1979). Secondary Ca–Al silicates as lowgrade alteration products of granitoid biotite. Contribuitions to Mineralogy and Petrology, 69(2), 105-117. https://doi.org/10.1007/BF00371854

Van Schmus, W. R., Oliveira, E. P., Silva Filho, A., Toteu, S. F., Penaye, J., Guimarães, I. P. (2008). Proterozoic Links between the Borborema Province NE Brazil and the Central African Fold Belt. Geological Society London Special Publication, 294, 69-99. https://doi.org/10.1144/SP294.5

Van Schmus, W. R., Kozuch, M., Brito Neves, B. B. (2011). Precambrian history of the Zona Transversal of the Borborema Province, NE Brazil: Insights from Sm-Nd and U-Pb geochronology. Journal of South American Earth Sciences, 31(2-3), 227-252. https://doi.org/10.1016/j.jsames.2011.02.010

Wones, D. R. (1989). Significance of the assemblage titanite + magnetite + quartz in granitic rocks. American Mineralogist, 74(7-8), 744-749.

Zen, E.-A., Hammarstrom, J. M. (1984). Magmatic epidote and its petrologic significance. Geology, 12(9), 515-518. https://doi.org/10.1130/0091-7613(1984)12<515:MEAIPS>2.0.CO;2

Petrology of Serra da Vaca Stock, Poço Redondo Domain, Sergipano Orogenic System

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