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Campo DCValorIdioma
dc.contributor.authorMedeiros, Rodrigo Jesus de-
dc.date.accessioned2026-07-20T19:34:37Z-
dc.date.available2026-07-20T19:34:37Z-
dc.date.issued2026-04-24-
dc.identifier.citationGARCIA, Rodrigo Medeiros Vieira. Processos físicos, petrogenéticos e geodinâmicos relacionados ao vulcanismo da sequência pré-sal na porção central da Bacia de Santos. 2026. 95 f. Dissertação (Mestrado em Geociências) - Instituto de Geociências, Universidade Federal Rural do Rio de Janeiro, Seropédica, RJ, 2026.pt_BR
dc.identifier.urihttp://rima.ufrrj.br/jspui/handle/20.500.14407/25825-
dc.description.abstractOs maiores volumes de reservas de petróleo e gás do Brasil ocorrem na sequência sedimentar do Cretáceo Inferior abaixo de uma espessa camada evaporítica na Bacia de Santos. Associadas a essa sequência pré-sal, ocorrem rochas magmáticas máficas intercaladas aos principais intervalos geradores e reservatórios, cuja gênese e papel no sistema petrolífero ainda não são plenamente compreendidos. O magmatismo pré-sal está relacionado à evolução tectônica da bacia durante a fragmentação do Gondwana e persistiu até o Aptiano Superior, ao longo do estágio sag, sendo tradicionalmente interpretado com base em dados geofísicos, com uso limitado de informações petrológicas e geoquímicas em modelos petrogenéticos e geodinâmicos. Esta dissertação apresenta um estudo petrológico integrado de amostras de testemunhos laterais recuperadas de dois poços localizados nas porções norte e sul da região central da Bacia de Santos. As rochas estudadas correspondem a basaltos toleíticos de alto e baixo teor de Ti, cujos episódios eruptivos ocorreram de forma sincrônica aos processos sedimentares responsáveis pela formação dos principais reservatórios pré-sal. A investigação envolveu análises petrográficas, geoquímicas de elementos maiores, traço e terras raras, além de modelagens petrogenéticas, com o objetivo de reconstruir os processos magmáticos, os estilos vulcânicos e os cenários geodinâmicos associados. Os resultados indicam que os basaltos toleíticos de alto Ti, na porção norte da área de estudo, correspondem a um único derrame basáltico espesso, com aproximadamente 48 m de espessura. Em contraste, os basaltos toleíticos de baixo Ti, na porção sul, registram múltiplos episódios vulcânicos, incluindo eventos efusivos e explosivos, alimentados por pelo menos seis fontes magmáticas subvulcânicas distintas ao longo de três eventos vulcânicos separados por períodos de quiescência sedimentar. A modelagem petrogenética sugere que ambos os grupos de basaltos derivam de diferentes graus de fusão parcial de uma fonte mantélica comum. Os dados geoquímicos e os resultados das modelagens são compatíveis com um cenário geodinâmico envolvendo a interação entre uma astenosfera rasa enriquecida e o manto litosférico subcontinental durante os estágios iniciais do rifteamento do Gondwana. Não há evidências diretas de contribuição de magmas derivados de uma pluma mantélica, embora sua possível presença em níveis mais profundos possa ter fornecido o aporte térmico necessário para promover a fusão parcial do manto raso. Esse regime magmático implica um elevado gradiente geotérmico durante a formação do sistema petrolífero pré-sal na Bacia de Santos.pt_BR
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESpt_BR
dc.languageporpt_BR
dc.publisherUniversidade Federal Rural do Rio de Janeiropt_BR
dc.subjectBacia de Santospt_BR
dc.subjectPré-salpt_BR
dc.subjectMagmatismopt_BR
dc.subjectSantos Basilpt_BR
dc.subjectPre-saltpt_BR
dc.subjectMagmatismpt_BR
dc.titleProcessos físicos, petrogenéticos e geodinâmicos relacionados ao vulcanismo da sequência pré-sal na porção central da Bacia de Santospt_BR
dc.title.alternativePhysical, Petrogenetic, and Geodynamic Processes Related to the Volcanism of the Pre-Salt Sequence in the Central Portion of the Santos Basinen
dc.typeDissertaçãopt_BR
dc.description.abstractOtherThe largest volumes of oil and gas reserves in Brazil occur in the Lower Cretaceous sedimentary sequence beneath a thick evaporitic layer in the Santos Basin. Mafic magmatic rocks are associated with this pre-salt sequence, being interbedded with the main source and reservoir intervals, and their genesis and role in the petroleum system are still not fully understood. Pre-salt magmatism is related to the tectonic evolution of the basin during the breakup of Gondwana and persisted until the Late Aptian, throughout the sag stage, being traditionally interpreted mainly on the basis of geophysical data, with limited use of petrological and geochemical information in petrogenetic and geodynamic models. This dissertation presents an integrated petrological study of sidewall core samples recovered from two boreholes located in the northern and southern portions of the central Santos Basin. The studied rocks correspond to high- and low-Ti tholeiitic basalts, whose eruptive episodes occurred synchronously with the sedimentary processes responsible for the formation of the main pre-salt reservoirs. The investigation involved petrographic analyses, whole-rock geochemistry of major, trace and rare earth elements, and petrogenetic modeling, aiming to reconstruct magmatic processes, volcanic styles, and associated geodynamic scenarios. The results indicate that the high-Ti tholeiitic basalts in the northern part of the study area correspond to a single thick basalt flow, approximately 48 m in thickness. In contrast, the low-Ti tholeiitic basalts in the southern portion record multiple volcanic episodes, including effusive and explosive events, fed by at least six distinct subvolcanic magmatic sources during three volcanic events separated by periods of sedimentary quiescence. Petrogenetic modeling suggests that both basalt groups were derived from different degrees of partial melting of a common mantle source. Geochemical data and modeling results are consistent with a geodynamic scenario involving interactions between a shallow, enriched asthenosphere and the subcontinental lithospheric mantle during the early stages of Gondwana rifting. There is no direct evidence for the contribution of melts derived from a mantle plume, although its possible presence at deeper levels may have provided the thermal input required to promote partial melting of the shallow mantle. This magmatic regime implies a high geothermal gradient during the formation of the pre-salt petroleum system in the Santos Basin.en
dc.contributor.advisor1Valente, Sergio de Castro-
dc.contributor.advisor1IDhttps://orcid.org/0000-0002-7467-672Xpt_BR
dc.contributor.advisor1Latteshttp://lattes.cnpq.br/7049948512331299pt_BR
dc.contributor.advisor-co1Rosseti, Marcos de Magalhães May-
dc.contributor.advisor-co1Lattes-pt_BR
dc.contributor.referee1Valente, Sergio de Castro-
dc.contributor.referee1IDhttps://orcid.org/0000-0002-7467-672Xpt_BR
dc.contributor.referee1Latteshttp://lattes.cnpq.br/7049948512331299pt_BR
dc.contributor.referee2Rossetti, Marcos de Magalhães May-
dc.contributor.referee2Lattes-pt_BR
dc.contributor.referee3Marins, Gabriel Medeiros-
dc.contributor.referee3Latteshttp://lattes.cnpq.br/3516572104740702pt_BR
dc.contributor.referee4Silva, Júlio César Lopes da-
dc.contributor.referee4IDhttps://orcid.org/0000-0001-6230-0058pt_BR
dc.contributor.referee4Latteshttp://lattes.cnpq.br/4978515572360716pt_BR
dc.creator.Latteshttp://lattes.cnpq.br/8788197899545402pt_BR
dc.publisher.countryBrasilpt_BR
dc.publisher.departmentInstituto de Geociênciaspt_BR
dc.publisher.initialsUFRRJpt_BR
dc.publisher.programPrograma de Pós-graduação em Modelagem e Evolução Geológicapt_BR
dc.relation.referencesAbdelmalak, M.M.; Jerram, D.A.; Rossetti, L.M.; Faleide, J.I.; Millett, J.M.; Polteau, S. (2025). Breakup magmatism in the South Atlantic: Mechanisms and implications. Earth-Science Reviews, 264, 105088. https://doi.org/10.1016/j.earscirev.2025.105088 Almeida, C.N.; Negri, F.A.; Mendes, J.C.; Miranda, A.; Valente, S.C.; Vieira, A.C.; Medeiros, S.R.; Borghi, L.; Miloski, P.; Cardoso, M.; Godot, J. (2025). High- and Low-Ti tholeiites in the Eastern Parnaíba Basin: Regional correlations with Mesozoic large igneous provinces. Brazilian Journal of Geology, 55, e20240037. https://doi.org/10.1590/2317-488920240037 81 Bagnardi, M.; Amelung, F.; Poland, M.P. (2013). A new model for the growth of basaltic shields based on deformation of Fernandina volcano, Galápagos Islands. Earth and Planetary Science Letters, 377–378, 358–366. https://doi.org/10.1016/j.epsl.2013.07.016 Bahlburg, H. & Dobrzinski, N. (2015). A review of the Chemical Index of Alteration (CIA) and its application to the study of Neoproterozoic glacial deposits and climate transitions. In: Arnaud, E.; Halverson, G.P.; Shields-Zhou, G. (eds.), The Geological Record of Neoproterozoic Glaciations. Geological Society, London, Memoirs, 36, 81–92. https://doi.org/10.1144/M36.6 Beccaluva, L.; Bianchini, G.; Natali, C.; Siena, F. (2020). Plume-related Paraná–Etendeka igneous province: An evolution from plateau to continental rifting and breakup. Lithos, 362– 363, 105484. https://doi.org/10.1016/j.lithos.2020.105484 Becerril, L.; Galindo, I.; Gudmundsson, A.; Morales, J.M. (2013). Depth of origin of magma in eruptions. Scientific Reports, 3, 2762. https://doi.org/10.1038/srep02762 Bergman, S.C. (1987). Lamproites and other potassium-rich igneous rocks: A review of their occurrence, mineralogy and geochemistry. Geological Society, London, Special Publications, 30, 103–190. https://doi.org/10.1144/GSL.SP.1987.030.01.08 Bertolini, G.; Hartley, A.J.; Marques, J.C.; Healy, D.; Frantz, J.C. (2021). The effects of basaltic lava flows on the petrophysical properties and diagenesis of interbedded aeolian sandstones: An example from the Cretaceous Paraná Basin, Brazil. Petroleum Geoscience, 27(2). https://doi.org/10.1144/petgeo2020-036 Binde, C.M.; Manton, B.; Plaza-Faverola, A.; Bünz, S.; Planke, S. (2025). Seismic characteristics and morphology of an igneous intrusion in the Vøring Basin, offshore Norway: New insights on the lateral evolution of elongated intrusions. Geochemistry, Geophysics, Geosystems, 26, e2025GC012429. https://doi.org/10.1029/2025GC012429 Boyd, F.R. & Mertzman, S.A. (1987). Composition and structure of the Kaapvaal lithosphere, Southern Africa. In: Mysen, B.O. (Ed.), Magmatic processes: Physicochemical principles; a volume in honor of Hatten S. Yoder,Jr., Geochemical Society, University Park, PA, pp. 13–24. Burchardt, S. (2018). Introduction to volcanic and igneous plumbing systems: developing a discipline and common concepts. In: Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth’s Crust. Uppsala: Elsevier, p. 1–12. https://doi.org/10.1016/B978-0-12-809749-6.00001-7 Burchardt, S.; Tanner, D.C.; Troll, V.R.; Krumbholz, M.; Gustafsson, L.E. (2011). Three- dimensional geometry of concentric intrusive sheet swarms in the Geitafell and the Dyrfjöll volcanoes, eastern Iceland. Geochemistry, Geophysics, Geosystems, 12, Q0AB09. https://doi.org/10.1029/2011GC003527 Cañón-Tapia, E. (2022). Plateau basalts (AKA flood basalts). In: Hargitai, H.; Kereszturi, Á. (eds.), Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_724-1 Carof, M. (1995). Open system crystallization and mixing in two-layer magma chambers. Lithos, 36, 85–102. Carvas, K.Z.; Vasconcelos, P.M.P.; Marques, L.S.; Ubide, T.; Carmo, I.O.; Babinski, M. (2021). Geochronology of mafic magmatism and hydrothermal alteration during early stages of South Atlantic opening. Geochimica et Cosmochimica Acta, 314, 358–380. https://doi.org/10.1016/j.gca.2021.08.017 82 Cashman, K.V. & Sparks, R.S.J. (2013). How volcanoes work: A 25-year perspective. GSA Bulletin, 125(5–6). https://doi.org/10.1130/B30720.1 Chang, H.K., Kowsmann, R.O., Figueiredo, A.M.F., & Bender, A.A. (1992). Tectonics and stratigraphy of the East Brazil Rift system: an overview. Tectonophysics, 213, 97–138. Chang, H.K.; Assine, M.L.; Corrêa, F.S.; Tinen, J.S.; Vidal, A.C.; Koike, L. (2008). Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos. Revista Brasileira de Geociências, 38(2 – supl.), 29–46. Cho, T. & Ohta, T. (2022). A robust chemical weathering index for sediments containing authigenic and biogenic materials. Palaeogeography, Palaeoclimatology, Palaeoecology, 608, 111288. https://doi.org/10.1016/j.palaeo.2022.111288 Coote, A.; Shane, P.; Fu, B. (2019). Olivine phenocryst origins and mantle magma sources for monogenetic basal volcanoes in northern New Zealand from textural, geochemical and δ18O isotope data. Lithos, 344–345, 232–246. https://doi.org/10.1016/j.lithos.2019.06.026 Dani, A.P.O.; Remus, M.V.D.; Dani, N.; Lima, E.F. (2017). Basalt magmatism from Alagoas Stage (Campos Basin). Revista do Instituto de Geociências – USP, 17(2), 26–287. https://doi.org/10.11606/issn.2316-9095.v17-373 Dietterich, H.R.; Cashman, K.V. (2014). Channel networks within lava flows: Formation, evolution, and implications for flow behavior. Journal of Geophysical Research: Earth Surface, 119, 1704–1724. https://doi.org/10.1002/2014JF003103 Downes, H. (2001). Formation and modification of the shallow sub-continental lithospheric mantle: A review of geochemical evidence from ultramafic xenolith suites and tectonically emplaced ultramafic massifs of western and central Europe. Journal of Petrology, 42(1), 233– 250. https://doi.org/10.1093/petrology/42.1.233 Du, Y.; Cao, Y.; Zhang, Z.; Lou, Y. (2025). Petrology, geochronology, and geochemistry of Paleoproterozoic volcanic rocks in the Xiong’ershan area, NE China: Implication for petrogenesis and tectonic setting. International Geology Review, 1–21. https://doi.org/10.1080/00206814.2025.2555272 Duzgoren-Aydin, N.S.; Aydin, A.; Malpas, J. (2002). Re-assessment of chemical weathering indices: Case study on pyroclastic rocks of Hong Kong. Engineering Geology, 63, 99–119. https://doi.org/10.1016/S0013-7952(01)00073-4 Eggleton, R.A.; Foudoulis, C.; Varkevisser, D. (1987). Weathering of basalt: Changes in rock chemistry and mineralogy. Clays and Clay Minerals, 35(3), 161–169. https://doi.org/10.1346/CCMN.1987.0350301 Eldholm, O. & Grue, K. (1994). North Atlantic volcanic margins: Dimensions and production rates. Journal of Geophysical Research, 99(B2), 2955–2968. https://doi.org/10.1029/93JB02879 Elkins, L.J.; Gaetani, G.A.; Sims, K.W.W. (2008). Partitioning of U and Th during garnet pyroxenite partial melting: Constraints on the source of alkaline ocean island basalts. Earth and Planetary Science Letters, 265, 270–286. https://doi.org/10.1016/j.epsl.2007.10.034 Famelli, N.; Millett, J.; Oliveira, L.C.; Hole, M.; Lima, E.F.; Jerram, D.A.; Carmo, I.O.; Planke, S.; Pugsley, J.H.; Chmielewska, M.; Howell, J.A.; Jolley, D.W. (2024). Understanding the petrophysical properties, seismic responses and impacts of the basalt-sediment transition in 83 prospective sedimentary basins. Journal of South American Earth Sciences, 148, 105113. https://doi.org/10.1016/j.jsames.2024.105113 Ferreira, L.C.; Stanton, N.; Gordon, A.C.; Schmitt, R. (2023). The magmatic rifting of Santos Basin: Aeromagnetic mapping of dykes, terranes and marginal structures and the interplay between tectonism and volcanism. Tectonics. https://doi.org/10.1029/2022TC007560 Florisbal, L.M.; Janasi, V.A.; Bitencourt, M.F.; Nardi, L.V.S.; Marteleto, N.S. (2018). Geological, geochemical and isotope diversity of ~134 Ma dykes from the Florianópolis Dyke Swarm, Paraná Magmatic Province: Geodynamic controls on petrogenesis. Journal of Volcanology and Geothermal Research, 355, 181–203. https://doi.org/10.1016/j.jvolgeores.2017.08.002 Floyd, P.A. & Winchester, J.A. (1978). Identification and discrimination of altered and metamorphosed volcanic rocks using immobile elements. Chemical Geology, 21, 291–306. Fodor, R.V. & Vetter, S.K. (1984). Rift-zone magmatism: Petrology of basaltic rocks transitional from CFB to MORB, southeastern Brazil margin. Contributions to Mineralogy and Petrology, 88, 307–321. Fornero, S.A.; Marins, G.M.; Lobo, J.T.; Freire, A.F.M.; Lima, E.F. (2019). Characterization of subaerial volcanic facies using acoustic image logs: Lithofacies and log-facies of a lava-flow deposit in the Brazilian Pre-Salt, deepwater Santos Basin. Marine and Petroleum Geology, 99, 156–174. https://doi.org/10.1016/j.marpetgeo.2018.09.029 Freitas, V.A.; Vital, J.C.S.; Rodrigues, B.R.; Rodrigues, R. (2022). Source rock potential, main depocenters, and CO2 occurrence in the Pre-Salt section of Santos Basin, southeast Brazil. Journal of South American Earth Sciences, 115, 103760. https://doi.org/10.1016/j.jsames.2022.103760 Frey, F.A. (1969). Rare earth abundances in a high-temperature peridotite intrusion. Geochimica et Cosmochimica Acta, 33, 1429–1447. https://doi.org/10.1016/0016- 7037(69)90183-5 Galland, O.; Villar, H.J.; Mescua, J.; Jerram, D.A.; Messager, G.; Medialdea, A.; Midtkandal, I.; Palma, J.O.; Planke, S.; Augland, L.E.; Zanella, A. (2024). Structural control of igneous intrusions on fluid migration in sedimentary basins: the case study of large bitumen seeps at Cerro Alquitrán and Cerro La Paloma, northern Neuquén Basin, Argentina. The Impacts of Igneous Systems on Sedimentary Basins and their Energy Resources. https://doi.org/10.1144/SP547-2023-115 Garda, M.G. (1995). Os diques básicos e ultrabásicos da região costeira entre as cidades de São Sebastião e Ubatuba, estado de São Paulo. Tese de Doutorado. Gibson, S.A.; Thompson, R.N.; Leonardos, O.H.; Dickin, A.P.; Mitchell, J.G. (1995). The Late Cretaceous impact of the Trindade mantle plume: Evidence from large-volume, mafic, potassic magmatism in SE Brazil. Journal of Petrology, 36(1), 189–229. https://doi.org/10.1093/petrology/36.1.189 Gomes, A.S. & Vasconcelos, P.M. (2021). Geochronology of the Paraná–Etendeka large igneous province. Earth-Science Reviews, 220, 103716. https://doi.org/10.1016/j.earscirev.2021.103716 Gordon, A.C.; Mohriak, W.U.; Stanton, N.; Santos, A.C. (2023). Magmatic cycles in Santos Basin (S.E. Brazil): Tectonic control in the temporal-spatial distribution and geophysical 84 signature. Journal of South American Earth Sciences. https://doi.org/10.1016/j.jsames.2022.104111 Greeley, R. (1977). Basaltic “plains” volcanism. In: Greeley, R.; King, J.S. (eds.), Volcanism of the Eastern Snake River Plain, Idaho: A comparative planetary guidebook. NASA, Washington, DC, 24–44. Green, D.H. (1970). A review of experimental evidence on the origin of basaltic and nephelinitic magmas. Physics of the Earth and Planetary Interiors, 3, 221–235. https://doi.org/10.1016/0031- 9201(70)90060-9 Green, D.H. (2015). Experimental petrology of peridotites, including effects of water and carbon on melting in the Earth’s upper mantle. Physics and Chemistry of Minerals, 42, 95–122. https://doi.org/10.1007/s00269-014-0729-2 Gudmundsson, A. & Lotveit, I. (2014). Sills as fractured hydrocarbon reservoirs: Examples and models. Geological Society, London, Special Publications, 374, 113–136. https://doi.org/10.1144/SP374.5 Harris, C.; Luttinen, A.; Howarth, G.H. (2025). The Karoo Large Igneous Province. South African Journal of Geology. https://doi.org/10.25131/sajg.129.1.2741 Harry, D.L. & Leeman, W.P. (1995). Partial melting of melt metasomatized subcontinental mantle and the magma source potential of the lower lithosphere. Journal of Geophysical Research, 100(B7), 10255–10269. Hawkesworth, C.J.; Gallagher, K.; Kirstein, L.; Mantovani, M.S.M.; Peate, D.W.; Turner, S.P. (2000). Tectonic controls on magmatism associated with continental break-up: An example from the Paraná–Etendeka Province. Earth and Planetary Science Letters, 179, 335–349. He, W.; Wang, H.; Su, J.; Wang, W.; Zhao, J.; Zuo, G.; Wang, T.; Yang, L.; Ren, K.; Wang, C.; Zhao, J.; Guo, Y.; Zhang, Y.; Sun, J. (2025). Magma evolution during the post-rift phase of the Santos Basin, Brazil: Petrogenesis and geochemistry of ∼126–121 Ma basalts and diabases. Frontiers in Earth Science, 12, 1497913. https://doi.org/10.3389/feart.2024.1497913 Hertogen, J. & Gijbels, R. (1976). Calculation of trace element fractionation during partial melting. Geochimica et Cosmochimica Acta, 40(3), 313–322. https://doi.org/10.1016/0016- 7037(76)90209-X Higuchi, H. & Nagasawa, H. (1969). Partition of trace elements between rock-forming minerals and the host volcanic rocks. Earth and Planetary Science Letters, 7, 281–287. https://doi.org/10.1016/0012-821X(69)90066-1 Hirose, K.; Kawamoto, T. (1995). Hydrous partial melting of lherzolite at 1 GPa: The effect of H2O on the genesis of basaltic magmas. Earth and Planetary Science Letters, 133, 463–473. https://doi.org/10.1016/0012-821X(95)00096-U Hirose, K.; Kawamura, K. (1994). A new experimental approach for incremental batch melting of peridotite at 1.5 GPa. Geophysical Research Letters. https://doi.org/10.1029/94GL01792 Hirschmann, M.M.; Ghiorso, M.S.; Stolper, E.M. (1999). Calculation of peridotite partial melting from thermodynamic models of minerals and melts. II. Isobaric variations in melts near the solidus and owing to variable source composition. Journal of Petrology, 40, 297–313. https://doi.org/10.1093/petroj/40.2.297 85 Hirschmann, M.M.; Ghiorso, M.S.; Wasylenki, L.E.; Asimow, P.D.; Stolper, E.M. (1998). Calculation of peridotite partial melting from thermodynamic models of minerals and melts. I. Review of methods and comparison with experiments. Journal of Petrology, 39, 1091–1115. https://doi.org/10.1093/petroj/39.6.1091 Hon, K.; Kauahikaua, J.; Denlinger, R.; Mackay, K. (1994). Emplacement and inflation of pahoehoe sheet flows: Observations and measurements of active lava flows on Kilauea Volcano, Hawaii. GSA Bulletin, 106(3), 351–370. https://doi.org/10.1130/0016- 7606(1994)106<0351:EAIOPS>2.3.CO;2 Horn, B.L.D.; Oliveira, A.A.; Simões, M.S.; Besser, M.L.; Araújo, L.L. 2022. Projeto Geologia e Potencial Mineral da Bacia do Paraná. Mapa geológico. Porto Alegre. SGB/CPRM. Escala 1:1000000. Howarth, G.H. & Harris, C. (2017). Discriminating between pyroxenite and peridotite sources for continental flood basalts (CFB) in southern Africa using olivine chemistry. Earth and Planetary Science Letters, 475, 143–151. https://doi.org/10.1016/j.epsl.2017.07.043 Humphris, S.E. & Thompson, G. (1978a). Trace element mobility during hydrothermal alteration of oceanic basalts. Geochimica et Cosmochimica Acta, 42, 127–136. Humphris, S.E. & Thompson, G. (1978b). Hydrothermal alteration of oceanic basalts by seawater. Geochimica et Cosmochimica Acta, 42, 107–125. Irving, A.J.; Frey, A. (1984). Trace element abundances in megacrysts and their host basalts: Constraints on partition coefficients and megacryst genesis. Geochimica et Cosmochimica Acta, 48, 1201–1221. https://doi.org/10.1016/0016-7037(84)90056-5 Ivanov, A.V. (2015). Why volatiles are required for cratonic flood basalt volcanism: Two examples from the Siberian craton. In: The Interdisciplinary Earth: A Volume in Honor of Don L. Anderson. (Foulger, G.R.; Lustrino, M.; King, S.D., eds.). James, D.E.; Boyd, F.R.; Schutt, D.; Bell, D.R.; Carlson, R.W. (2004). Xenolith constraints on seismic velocities in the upper mantle beneath southern Africa. Geochemistry, Geophysics, Geosystems, 5, Q01002. https://doi.org/10.1029/2003GC000551 Jerram, D.A., Mountney, N.P., Howell, J.A., Long, D., & Stollhofen, H. (2000). Death of a sand sea: an active aeolian erg systematically buried by the Etendeka flood basalts of NW Namibia. Journal of the Geological Society, 157, 513–516. https://doi.org/10.1144/jgs.157.3.513 Jerram, D. A. (2002). Volcanology and facies architecture of flood basalts. Geological Society of America Special Paper 362 2002. Department of Geological Sciences, University of Durham. Jerram, D.A. & Widdowson, M. (2005). The anatomy of continental flood basalt provinces: Geological constraints on the processes and products of flood volcanism. Lithos, 79(3–4), 385– 405. Jung, S.; Romer, R.L.; Pfänder, J.A. (2025). Petrology of alkali gabbro from the Messum Crater, Namibia (Paraná–Etendeka Province): Melting of metasomatized carbonated lithospheric mantle sources. Chemical Geology, 673, 122547. https://doi.org/10.1016/j.chemgeo.2024.122547 Karátson, D. & Thouret, J.C. (2025). Volcano Geomorphology: Landforms, Processes, and Hazards. Advances in Volcanology. Chapter 1: Spatial distribution and tectonic setting of volcanoes. https://doi.org/10.1007/978-3-031-77693-9 86 Keating, G.N.; Valentine, G.A.; Krier, D.J.; Perry, F.V. (2008). Shallow plumbing systems for small-volume basaltic volcanoes. Bulletin of Volcanology, 70, 563–582. Krein, S.B.; Molitor, Z.J.; Grove, T.L. (2021). Reverse Petrogen: A multiphase dry reverse fractional crystallization–mantle melting thermobarometer applied to 13,589 mid-ocean ridge basalt glasses. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/2020JB021292 Kushiro, I. (2001). Partial melting experiments on peridotite and origin of mid -ocean ridge basalt. Annual Review of Earth and Planetary Sciences, 29, 71–107. https://doi.org/10.1146/annurev.earth.29.1.71 Lang, S.; Mollo, S.; France, L.; Misiti, V.; Nazzari, M. (2021). Kinetic partitioning of major- minor cations between olivine and Hawaiian tholeiitic basalt under variable undercooling and cooling rate conditions. Chemical Geology, 584, 120485. https://doi.org/10.1016/j.chemgeo.2021.120485 Lima, B.E.M. & De Ros, L.F. (2019). Deposition, diagenetic and hydrothermal processes in the Aptian Pre-Salt lacustrine carbonate reservoirs of the northern Campos Basin, offshore Brazil. Sedimentary Geology, 383, 55–81. https://doi.org/10.1016/j.sedgeo.2019.01.006 Lindsay, J.J.; Hughes, H.S.R.; Yeomans, C.M.; Andersen, J.C.Ø.; McDonald, I. (2021). From continent to ocean: Investigating the multi-element and precious metal geochemistry of the Paraná–Etendeka Large Igneous Province using machine learning tools. Earth Science, Systems and Society, 1, 10039. https://doi.org/10.3389/esss.2021.10039 Liu, Q.; Zhu, D.; Jin, Z.; Meng, Q.; Wu, X.; Yu, H. (2017). Effects of deep CO2 on petroleum and thermal alteration: The case of the Huangqiao oil and gas field. Chemical Geology, 469, 214–229. https://doi.org/10.1016/j.chemgeo.2017.06.031 Louback, V.S.; Valente, S.C.; Almeida, C.N.; Ross, J.; Borghi, L. (2023). Aptian flood basalts in Bacalhau oil and gas field: Petrogenesis and geodynamics of post-rift tholeiites in the Pre- Salt sequence of Santos Basin, Brazil. Contributions to Mineralogy and Petrology, 178, 15. https://doi.org/10.1007/s00410-023-01995-0 Louback, V.S.; Valente, S.C.; Almeida, C.N.; Ross, J.; Borghi, L. (2021). Petrogenesis and geodynamics of Eocene alkaline intrusions in the Pre-Salt sedimentary sequence of Santos Basin, Brazil. Lithos, 400–401, 106400. https://doi.org/10.1016/j.lithos.2021.106400 Lovecchio, J.P., Abdelmalak, M.M., Planke, S., Silio, O., Rohais, S., Arismendi, S., Rojas Vera, E., Kulhanek, D.K., Bolatti, N., & Ramos, V.A. (2024). Mesozoic rifting in SW Gondwana and break-up of the Southern South Atlantic Ocean. Geological Society, London, Special Publications, 547. https://doi.org/10.1144/SP547-2023-140 Magee, C.; Pichel, L.M.; Madden-Nadeau, A.L.; Jackson, C.A.L.; Mohriak, W. (2021). Salt– magma interactions influence intrusion distribution and salt tectonics in the Santos Basin, offshore Brazil. Basin Research, 33, 1820–1843. https://doi.org/10.1111/bre.12537 Mahiques, M.M.; Schattner, U.; Riccomini, C.; Janasi, V.A.; Lobo, F.J.; Vasconcelos, P.; Thiede, D.S.; Ramos, R.B.; Santos, R.F. (2023). Submarine basalt xenoliths confirm the occurrence of post-rift volcanism in the southern Santos Basin, SW Atlantic. Journal of South American Earth Sciences, 132, 104661. https://doi.org/10.1016/j.jsames.2023.104661 Marins, G.M.; Parizek-Silva, Y.; Millett, J.M.; Jerram, D.A.; Rossetti, L.M.M.; Souza, A.J.; Planke, S.; Bevilaqua, L.A.; Carmo, I.O. (2022). Characterization of volcanic reservoirs: 87 Insights from the Badejo and Linguado oil fields, Campos Basin, Brazil. Marine and Petroleum Geology, 146, 105950. https://doi.org/10.1016/j.marpetgeo.2022.105950 Mathieu, L. (2018). Quantifying hydrothermal alteration: A review of methods. Geosciences, 8(7), 245. https://doi.org/10.3390/geosciences8070245 Matzen, A.K.; Baker, M.B.; Beckett, J.R.; Wood, B.J.; Stolper, E.M. (2017). The effect of liquid composition on the partitioning of Ni between olivine and silicate melt. Contributions to Mineralogy and Petrology, 172, 3. https://doi.org/10.1007/s00410-016-1319-8 McDonough, W.F. & Sun, S.S. (1995). The composition of the Earth. Chemical Geology, 120(3–4), 223–253. https://doi.org/10.1016/0009-2541(94)00140-4 McKenzie, D. & O’Nions, R.K. (1991). Partial melt distributions from inversion of rare earth element concentrations. Journal of Petrology, 32(5), 1021–1091. https://doi.org/10.1093/petrology/32.5.1021 Mello, M.R.; Peres, W.; Rostirolla, S.P.; Pedrosa, O.A.; Piquet, A.; Becker, S.; Yilmaz, P.O. (2021). The Santos Basin Pre-Salt Super Giant Petroleum System: An incredible journey from failure to success. In: Memoir 124 – The Supergiant Lower Cretaceous Pre-Salt Petroleum Systems of the Santos Basin, Brazil, pp. 1–34. https://doi.org/10.1306/13722313MSB.1.1853 Meunier, A.; Caner, L.; Hubert, F.; Albani, A.; Pret, D. (2013). The weathering intensity scale (WIS): An alternative approach to the chemical index of alteration (CIA). American Journal of Science, 313, 113–143. https://doi.org/10.2475/02.2013.03 Millett, J.M.; Jolley, D.W.; Hole, M.J.; Augland, L.; Pugsley, J.H.; McLeod, G.W.; Planke, S. (2024). High-precision U–Pb zircon dating of explosive volcanism in an early bimodal volcano- sedimentary sequence from the Isle of Mull, North Atlantic Igneous Province. Lithos, 482–483, 107729. https://doi.org/10.1016/j.lithos.2024.107729 Mizusaki, A.M.P.; Petrini, R.; Bellieni, G.; Comin-Chiaramonti, P.; Dias, J.; De Min, A.; Picerillo, E.M. (1992). Basalt magmatism along the passive continental margin of SE Brazil (Campos Basin). Contributions to Mineralogy and Petrology, 111, 143–160. Mohriak, W.U. & Szameitat, L. (2023). The anomalous magmatism in the southern part of the Santos Basin, and the non-continuoussalt layer over Abimael Ridge.Journal of South American Earth Sciences, 128, 104435. https://doi.org/10.1016/j.jsames.2023.104435 Moreira, J.L.P., Madeira, C.L., Gil, J.A., & Machado, M.A.P. (2007). Bacia de Santos. Boletim de Geociências - Petrobras, 15, 531–549. Moreira, J.L.P.; Esteves, C.A.; Rodrigues, J.J.G.; Vasconcelos, C.S. (2006). Magmatismo, sedimentação e estratigrafia da porção norte da Bacia de Santos. Boletim de Geociências – Petrobras, 14, 161–170. Mottl, M.J. & Holland, H.D. (1978). Chemical exchange during hydrothermal alteration of basalt by seawater—I: Experimental results for major and minor components of seawater. Geochimica et Cosmochimica Acta, 42(8), 1103–1115. https://doi.org/10.1016/0016- 7037(78)90107-2 Mou, J.L.; Lee, C.T.; Borchardt, J. (2025). Calibrating olivine Forsterite content as a measure of melting degree in residual peridotites. Geochimica et Cosmochimica Acta. https://doi.org/10.1016/j.gca.2025.08.021 88 Nagasawa, H.; Schreiber, H.D.; Morris, R.V. (1980). Experimental mineral/liquid partition coefficients of the rare earth elements (REE), Sc and Sr for perovskite, spinel and melilite. Earth and Planetary Science Letters, 46(3), 431–437. https://doi.org/10.1016/0012-821X(80)90056- 4 Nagasawa, H.; Wakita, H.; Higuchi, H.; Onuma, N. (1968). Rare earths in peridotite nodules: An explanation of the genetic relationship between basalt and peridotite nodules. Earth and Planetary Science Letters, 5, 377–381. https://doi.org/10.1016/S0012-821X(68)80067-6 Natali, C.; Beccaluva, L.; Bianchini, G.; Siena, F. (2017). Comparison among Ethiopia–Yemen, Deccan, and Karoo continental flood basalts of central Gondwana: Insights on lithosphere versus asthenosphere contributions in compositionally zoned magmatic provinces. In: The Crust–Mantle and Lithosphere–Asthenosphere Boundaries. https://doi.org/10.1130/2017.2526(10) Nesbitt, H.W. & Young, G.M. (1984). Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochimica et Cosmochimica Acta, 48, 1523–1534. https://doi.org/10.1016/0016-7037(84)90408-3 Neves, I.A.; Lupinacci, W.M.; Ferreira, D.J.A.; Zambrini, J.P.R.; Oliveira, L.O.A.; Azul, M.O.; Ferrari, A.L.; Gamboa, L.A.P. (2019). Presalt reservoirs of the Santos Basin: Cyclicity, electrofacies, and tectonic-sedimentary evolution. Interpretation, 7(4), SH33–SH43. https://doi.org/10.1190/INT-2018-0237.1 O’Hara, M.J. (1977). Geochemical evolution during fractional crystallization of a periodically refilled magma chamber. Nature, 266, 503–507. Ohta, T. & Arai, H. (2007). Statistical empirical index of chemical weathering in igneous rocks: A new tool for evaluating the degree of weathering. Chemical Geology, 240, 280–297. https://doi.org/10.1016/j.chemgeo.2007.02.017 Oliveira, F.V.C.S.R.S.; Carmo, I.O.; Costa, J.; Bittencourt, B.T.; Lupinacci, W.M.; Freire, A.F. (2024). Characterization of subaerial lava flows of the presalt strata in the Santos Basin based on basic well logs. Journal of South American Earth Sciences, 139, 104884. https://doi.org/10.1016/j.jsames.2024.104884 Oliveira, F.V.C.S.R.S.; Gomes, R.T.M.; Silva, K.M.S. (2019). Log features for the characterization of igneous rocks in the Pre-Salt area of Santos Basin, SE Brazil. Search and Discovery, 11264. https://doi.org/10.1306/11264Oliveira2019 Oliveira, L.C.; Penna, R.M.; Rancan, C.C.; Carmo, I.O.; Marins, G.M. (2024). Seismic interpretation of the Mero Field igneous rocks and its implications for pre- and post-salt CO2 generation – Santos Basin, offshore Brazil. Marine and Petroleum Geology, 163, 106775. https://doi.org/10.1016/j.marpetgeo.2024.106775 Oreiro, S.G.; Cupertino, A.; Szatmari, P.; Thomaz Filho, A. (2008). Influence of Pre-Salt alignments in post-Aptian magmatism in the Cabo Frio High and surroundings. Journal of South American Earth Sciences, 25, 116–131. Otto, T.; Stevens, G.; Moyen, J.-F.; Mayne, M.J.; Clemens, J.D. (2025). Peritectic orthopyroxene entrainment during partial melting of garnet peridotite produced the Bushveld Complex chromite deposits. Mineralium Deposita, 60, 289–301. https://doi.org/10.1007/s00126-024-01277-0 89 Pandey, A.; Gayathri, T.P.; Pang, K.-N.; Bhat, I.M.; Sachan, H.K. (2025). Geochemical insights into the origins of compositionally distinct Early Permian Panjal Traps basalts: Implications for the transition from continental lithospheric to sub-lithospheric mantle melting regimes. Geochemistry, 85, 126264. https://doi.org/10.1016/j.chemer.2025.126264 Parker, A. (1970). An index of weathering for silicate rocks. Geological Magazine. Paster, T.P.; Schauwecker, D.S.; Haskin, L.A. (1974). The behavior of some trace elements during solidification of the Skaergaard layered series. Geochimica et Cosmochimica Acta, 38, 1549–1577. https://doi.org/10.1016/0016-7037(74)90174-4 Paul, M.K.; Schwartz, D.M.; DuFrane, S.A.; et al. (2025). High-precision U–Pb dating and Hf isotopes of MARID zircons reveals multi-source, prolonged metasomatism of the Kaapvaal sub- continental lithospheric mantle. Mineralogy and Petrology. https://doi.org/10.1007/s00710-025-00915-3 Pearce, J.A. (1996). A user’s guide to basalt discrimination diagrams. In: Wyman, D.A. (ed.), Trace Element Geochemistry of Volcanic Rocks, 79–113. Peate, D.W. (1997). The Paraná–Etendeka Province. In Mahoney & Coffin (Eds.), Large Igneous Provinces. Geophysical Monograph 100. Penna, R., Araújo, S., Geisslinger, A., Sansonowski, R., Oliveira, L., Rosseto, J., Matos, M. (2019). Carbonate and igneous rock characterization. DOI: 10.1190/tle38010011.1. Piccirillo, E.M. & Melfi, A.J. (1988). The Mesozoic flood volcanism of the Paraná basin: petrogenetic and geophysical aspects. IAG-USP, São Paulo. 600pp. Planke, S.; Rasmussen, T.; Rey, S.S.; Myklebust, R. (2005). Seismic characteristics and distribution of volcanic intrusions and hydrothermal vent complexes in the Vøring and Møre basins. Petroleum Geology: North-West Europe and Global Perspectives, Proceedings of the 6th Petroleum Geology Conference, 833–844. Plawiak, R.A.B.; Carvalho, M.J.; Sombra, C.L.; Brandão, D.R.; Mepen, M.; Ferrari, A.L.; Gambôa, L.A.P. (2024). Structural controls of the migration of mantle-derived CO2 offshore in the Santos Basin (Southeastern Brazil). Frontiers in Earth Science, 11, 1284151. https://doi.org/10.3389/feart.2023.1284151 Price, R.C.; Gray, C.M.; Wilson, R.E.; Frey, F.A.; Taylor, S.R. (1991). The effects of weathering on rare-earth element, Y and Ba abundances in Tertiary basalts from southeastern Australia. Chemical Geology, 93(3–4), 245–265. Prinzhofer, A. & Allègre, C.J. (1985). Residual peridotites and the mechanisms of partial melting. Earth and Planetary Science Letters, 74, 251–265. Qin, Z. (1992). Disequilibrium partial melting model and its implications for trace element fractionations during mantle melting. Earth and Planetary Science Letters, 112, 75–90. https://doi.org/10.1016/0012-821X(92)90008-J Queiroz, B.S.; Valente, S.C.; Santos, A.C.; Heilbron, M. (2024). Petrophysical and petrographic data correlation and the discrimination of magmatic environments and processes in Santos Basin, offshore SE Brazil. Journal of South American Earth Sciences, 147, 105095. https://doi.org/10.1016/j.jsames.2024.105095 90 Queiroz, B.S.; Valente, S.C.; Santos, A.C.; Heilbron, M. (2025). Bimodal volcanism during the Early Cretaceous. Marine and Petroleum Geology. https://doi.org/10.1016/j.marpetgeo.2025.107495 Rancan, C.C.; Oliveira, L.C.;Carmo, I.O.; Marins, G.M.; Pessoa, V.C.O.; Andrade, H.; Penatti, A.P.R.; Borges, T.A.; Silva, R.C.B.; Carlotto, M.A.; Bassetto, M.; Zanatta, A.S. (2018). Rochas ígneas do Bloco de Libra, Bacia de Santos. 49o Congresso Brasileiro de Geologia, Rio de Janeiro. Regelous, M. (1993). Geochemistry of dolerites from the Paraná Flood Basalt Province, southern Brazil. Open University, ProQuest Dissertations & Theses, U554505. https://doi.org/10.21954/ou.ro.0000e04f Ren, K.; Oliveira, M.J.R.; Zhao, J.; Zhao, J.; Oliveira, L.C.; Rancan, C.C.; Carmo, I.O.; Deng, Q. (2019). Using wireline logging and thin sections to identify igneous contact metamorphism and hydrothermal influence on Pre-Salt limestone reservoirs in the Libra Block, Santos Basin. OTC-29818-MS, Offshore Technology Conference. Ren, K.; Zhao, J.; Liu, Q.; Zhao, J. (2020). Hydrocarbons in igneous rock of Brazil: A review. Petroleum Research, 5, 265–275. https://doi.org/10.1016/j.ptlrs.2020.06.001 Renne, P.R.; Ernesto, M.; Pacca, I.G.; Coe, R.S.; Glen, J.M.; Prévot, M.; Perrin, M. (1996). The age of Paraná flood volcanism, rifting of Gondwanaland, and the Jurassic–Cretaceous boundary. Science, 273(5282), 939–943. https://doi.org/10.1126/science.273.5282.939 Rock, N. M. S. (1987). The nature and origin of lamprophyres: an overview. Geological Society, London, Special Publications. Vol 30, Pag 191-226. https://doi.org/10.1144/GSL.SP.1987.030.01.09 Rodrigues, R.F.; Yaxley, G.M.; Kamber, B.S. (2025). Phase relations and solidus temperature of garnet lherzolite at 5 GPa revisited. Contributions to Mineralogy and Petrology, 180, 57. https://doi.org/10.1007/s00410-025-02250-4 Rodriguez, C.R.; Jackson, C.A.L.; Rotevatn, A.; Bell, R.E.; Francis, M. (2018). Dual tectonic- climatic controls on salt giant deposition in the Santos Basin, offshore Brazil. Geosphere, 14(1), 215–242. https://doi.org/10.1130/GES01434.1 Roeder, P.L. & Emslie, R.F. (1970). Olivine-liquid equilibrium. Contributions to Mineralogy and Petrology, 29, 275–289. Romero-Toribio, M.C.; Martín-Hernández, F.; Ledo, J. (2025). High-resolution drone-based aeromagnetic survey at the Tajogaite Volcano (La Palma, Canary Islands): Insights into its early post-eruptive shallow structure. Remote Sensing, 17, 3153. https://doi.org/10.3390/rs17183153 Salters, V.J.M. & Stracke, A. (2004). Composition of the depleted mantle. Geochemistry, Geophysics, Geosystems, 5, Q05B07. https://doi.org/10.1029/2003GC000597 Santos, R.O.R.; Bach, W.; Pérez-Gussinyé, M.; Araujo, M.N.C. (2026). Tholeiitic Magmatism in the Santos Basin: Evidence for Continental Setting and Its Connection to the Paraná-Etendeka Igneous Province. Versão ainda não avaliada por pares disponível em SSRN: https://ssrn.com/abstract=6390004 or http://dx.doi.org/10.2139/ssrn.6390004 Sarmento, C.C.T.; Sommer, C.A. ; Lima, E.F. ; Barreto, C.J.S. ; Rossetti, L.M.M.; Lafon, J.M. (2021). Mafic subvolcanic intrusions from the southern Paraná-Etendeka Large Igneous Province, Brazil: Insights from geochemistry and Sr–Nd–Pb isotopes. Geological Journal. 91 2021; 56: 1143–1166. https://doi.org/10.1002/gj.3993pt_BR
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