Artículos de revistas
Age, Composition, And Source Of Continental Arc- And Syn-collision Granites Of The Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil
Registro en:
Journal Of South American Earth Sciences. Elsevier Ltd, v. 58, n. , p. 257 - 280, 2015.
8959811
10.1016/j.jsames.2014.08.003
2-s2.0-84923079293
Autor
Oliveira E.P.
Bueno J.F.
McNaughton N.J.
Silva Filho A.F.
Nascimento R.S.
Donatti-Filho J.P.
Institución
Resumen
The Sergipano belt is the outcome of collision between the Pernambuco-Alagoas Domain (Massif) and the São Francisco Craton during Neoproterozoic assembly of West Gondwana. Although the understanding of the Sergipano belt evolution has improved significantly, the timing of emplacement, geochemistry and tectonic setting of granitic bodies in the belt is poorly known. We recognized two granite age groups: 630-618Ma granites in the Canindé, Poço Redondo and Macururé domains, and 590-570Ma granites in the Macururé metasedimentary domain. U-Pb SHRIMP zircon ages for granites of first age group indicated ages of 631±4Ma for the Sítios Novos granite, 623±7Ma for the Poço Redondo granite, 619±3.3Ma for the Lajedinho monzodiorite, and 618±3Ma for the Queimada Grande granodiorite. These granitoids are dominantly high-K calc-alkaline, magnesian, metaluminous, mafic enclave-rich (Queimada Grande and Lajedinho), or with abundant inherited zircon grains (Poço Redondo and Sitios Novos). Geochemical and isotope data allow us to propose that Sítios Novos and Poço Redondo granites are product of partial melting of Poço Redondo migmatites. Sr-Nd isotopes of the Queimada Grande granodiorite and Lajedinho monzodiorite suggest that their parental magma may have originated by mixing between a juvenile mafic source and a crustal component that could be the Poço Redondo migmatites or the Macururé metasediments. Other 630-618Ma granites in the belt are the mafic enclave-rich Coronel João Sá granodiorite and the Camará tonalite in the Macururé sedimentary domain. These granites have similar geochemical and isotopic characteristics as the Lajedinho and Queimada Grande granitoids. We infer for the Camará tonalite and Coronel João Sá granodiorite that their parental magmas have had contributions from mafic lower crust and felsic upper crust, most probably from underthrust São Francisco Craton, or Pernambuco-Alagoas Domain. The younger 590-570Ma granite group is confined to the Macururé metasedimentary domain. Although these granites do not show typical features of S-type granites, their U-Pb age, field relationships, geochemical and Sr-Nd data suggest that their parental magmas have originated from high degree melting of the Macururé micaschists. Field observations support a model in which the Macururé domain, limited by the Belo Monte-Jeremoabo and São Miguel do Aleixo shear zones, behaved as a ductile channel flow for magma migration and emplacement during the Neoproterozoic, very much like the channel flow model proposed for emplacement of leucogranites in the Himalayas. 58
257 280 Allard, G.O., Hurst, V.J., Brazil-Gabon geologic link supports continental drift (1969) Science, 163, pp. 528-532 Almeida, M.E., Macambira, M.J.B., Oliveira, E.C., Geochemistry and zircon geochronology of the I-type high-K calc-alkaline and S-type granitoid rocks from southeastern Roraima, Brazil: Orosirian collisional magmatism evidence (1.97-1.96 Ga) in central portion of Guyana Shield (2007) Precambrian Res., 155, pp. 69-97 Archanjo, C.J., Hollanda, M.H.B.M., Rodrigues, S.W.O., Neves, B.B.B., Armstrong, R., Fabrics of pre- and syntectonic granite plutons and chronology of shear zones in the Eastern Borborema Province, NE Brazil (2008) J.Struct. Geol., 30, pp. 310-326 Barbarin, B., Areview of the relationships between granitoid types, their origins and their geodynamic environments (1999) Lithos, 46, pp. 605-626 Bonin, B., From orogenic to anorogenic settings: evolution of granitoid suites after a major orogenesis (1990) Geol. J., 25, pp. 261-270 Briqueu, L., Bougault, H., Joron, J.L., Quantification of Nb, Ta, Ti and V anomalies in magmas associated with subduction zones - petrogenetic implications (1984) Earth Planet. Sci. Lett., 68, pp. 297-308 Brito Neves, B.B., Sial, A.N., Albuquerque, J.P.T., Vergência centrífuga residual no sistema de dobramentos Sergipano (1977) Rev. Bras. Geociências, 7, pp. 102-114 Brito Neves, B.B., Van Schmus, W.R., Santos, E.J., Campos Neto, M.C., Kozuch, M., OEvento Carirís Velhos na Província Borborema: Integração de Dados, Implicaço es e Perspectivas (1995) Rev. Bras. Geociências, 25, pp. 279-296 Brito Neves, B.B., Fuck, R.A., Neoproterozoic evolution of the basement of the South-American platform (2013) J. South Am. Earth Sci, 47, pp. 72-89 Bueno, J.F., Oliveira, E.P., McNaughton, N., Laux, J.H., 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 (2009) Gondwana Res., 15, pp. 86-97 Carvalho, M.J., (2005) Tectonic Evolution of the Marancó-Poç o Redondo Domain: Records of the Cariris Velhos and Brasiliano Orogenesis in the Sergipano Belt, NE Brazil, , Unpublished PhD thesis, University of Campinas, Brazil, 202 pp (in Portuguese) Chappell, B.W., White, A.J.R., Two contrasting granite type (1974) Pac. Geol., 8, pp. 173-174 Chappell, B.W., White, A.J.R., I- and S-types granites in Lachlan Fold Belt (1992) Trans. Royal Soc. Edinb. Earth Sci., 83, pp. 1-26 Chappell, B.W., White, A.J.R., Two contrasting granite types: 25 years later (2001) Aust. J. Earth Sci., 48, pp. 489-499 Clemens, J.D., S-type granitic magmas-petrogenetic issues, models and evidence (2003) Earth-Sci. Rev., 61, pp. 1-18 Compston, W., Williams, I.S., Meyer, C., U-Pb geochronology of zircons from lunar breccia 73217 using a sensitive high massresolution ion microprobe (1984) J. Geophys. Res., 89, pp. 252-534 Condie, K.C., Kröner, A., The building blocks of continental crust: evidence for a major change in the tectonic setting of continental growth at the end of the Archean (2013) Gondwana Res., 23, pp. 394-402 Cotta, A., Enzweiler, J., Quantification of major and trace elements in water samples by ICP-MS and collision cell to attenuate Ar and Cl-based polyatomic ions (2009) J.Anal. Atomic Spectrom., 24, pp. 1406-1413 Crawford, M.B., Searle, M.P., Collision-related granitoid magmatism and crustal structure of the Hunza Karakoram, North Pakistan (1993) Himalayan Tectonics, 74, pp. 53-68. , Geological Society Special Publication D'el-Rey Silva, L.J.H., The evolution of basement gneiss domes of the Sergipano fold belt (NE Brazil) and its importance for the analysis of Proterozoic basins (1995) J. South Am. Earth Sci., 8, pp. 325-340 Davison, I., Santos, R.A., Tectonic evolution of the Sergipano fold Belt, NE Brazil, during the Brasiliano orogeny (1989) Precambrian Res., 45, pp. 319-342 Debon, F., Le Fort, P., Achemical-mineralogical classification of common plutonic rocks and associations (1983) Trans. Royal Soc. Edinb. Earth Sci., 73, pp. 135-149 DePaolo, D.J., Neodymium isotopes in the Colorado Front Range and implications for crust formation and mantle evolution in the Proterozoic (1981) Nature, 291, pp. 193-197 Eggins, S.M., Woodhead, J.D., Kinsley, L.P.J., Mortimer, G.E., Sylvester, P., McCulloch, M.T., Hergt, J.M., Handler, M.R., Asimple method for the precise determination of > 40 trace elements in geological samples by ICPMS using enriched isotope internal standardisation (1997) Chem. Geol., 134, pp. 311-326 El Baghadadil, M., El Boukhari, A., Jouider, A., Benyoucef, A., Nadem, A., Calc-alkaline arc I-type Granitoid associated with S-type Granite in the Pan-African Belt of Eastern Anti-Atlas (Saghro and Ougnat, South Morocco) (2003) Gondwana Res., 6, pp. 557-572 Evensen, N.M., Hamilton, P.J., O'Nions, R.K., Rare earth abundances in chondritic meteorites (1978) Geochim. Cosmochim. Acta, 42, pp. 1199-1212 Ferré, E., Gleizes, G., Caby, R., Obliquely convergent tectonics and granite emplacement in the Trans-Saharan belt of Eastern Nigeria: a synthesis (2002) Precambrian Res., 114, pp. 199-219 Fetter, A.H., Santos, T.J.S., Van Schumus, W.R., Hackspacher, P.C., Brito Neves, B.B., Arthaud, M.H., Nogueira Neto, J.A., Wernick, E., Evidence for Neoproterozoic Continental arc magmatism in the Santa Quitéria Batholith of Ceará State, NW Borborerna Province, NE Brazil: Implications for the assembly of West Gondwana (2003) Gondwana Res., 6, pp. 265-273 Förster, H.J., Tischendorf, G., Trunbull, R.B., An evaluation of the Rb vs. (Y+Nb) discrimination diagram to infer tectonic setting of silicic igneous rocks (1997) Lithos, 40, pp. 261-293 Frost, B.R., Barnes, C.G., Collins, W.J., Arculus, R.J., Ellis, D.J., Frost, C.D., Ageochemical classification for granitic rocks (2001) J.Petrol., 42, pp. 2033-2048 Gioia, S.M.C.L., Pimentel, M.M., Sm-Nd isotopic method in the geochronology laboratory of University of Brasília (2000) An. Acad. Bras. Ciências, 72, pp. 219-245 Guimarães, I.P., Silva Filho, A.F., An example of in situ granite formation in the northern boundary of the Proterozoic Sergipano fold belt, NE Brazil: the Xingó Complex (1995) J.South Am. Earth Sci., 8, pp. 341-354 Guimarães, I.P., Silva Filho, A.F., Almeida, C.N., Van Schumus, W.R., Araújo, J.M.M., Melo, S.C., Melo, E.B., Brasiliano (Pan-African) granitic magmatism in the Pajeú-Paraíba belt, Northeast Brazil: an isotopic and geochronological approach (2004) Precambrian Res., 135, pp. 23-53 Karsli, O., Chen, B., Aydin, F., Sen, C., Geochemical and Sr-Nd-Pb isotopic compositions of the Eocene Dölek and Sariçiçek Plutons, Eastern Turkey: Implications for magma interaction in the genesis of high-K calc-alkaline granitoids in a post-collision extensional setting (2007) Lithos, 98, pp. 67-96 Klemperer, S.L., Crustal flow in Tibet: geophysical evidence for the physical state of Tibetan lithosphere, and inferred patterns of active flow (2006) Channel Flow, Ductile Extrusion and Exhumation in Continental Collision Zones, 268, pp. 39-70. , Geological Society, London, Special Publications (1989) Aclassification of igneous rocks and glossary of terms. Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks, p. 193. , Blackwell, Oxford, R.W. Le Maitre, P. Bateman, A. Dubek, J. Keller, J. Lameyre, M.J. Le Bas, P.A. Sabine, R. Schmid, H. Sørensen, A. Streckeisen, A.R. Woolley, B. Zanettin (Eds.) Leech, M.L., Singh, S., Jain, A.K., Klemperer, S.L., Manickavasagam, R.M., The onset of India-Asia collision: early, steep subduction required by timing of UHP metamorphism in the western Himalaya (2005) Earth Planet. Sci. Lett., 234, pp. 83-97 Liang, Q., Jing, H., Gregoire, D.C., Determination of trace elements in granites by inductively coupled plasma mass spectrometry (2000) Talanta, 51, pp. 507-513 Long, L.E., Castellana, C.H., Sial, A.N., Age, origin and cooling history of the Coronel João Sá Pluton, Bahia, Brazil (2005) J.Petrol., 46, pp. 255-273 Ludwig, K.R., (1999) Squid, Version 1.02, p. 16. , Center Spec. Pub., Berkeley Geochron, No. 2 Ludwig, K.R., (1999) Isoplot/Ex Version 2.00, a Geochronological Toolkit for Mircosoft Excel, p. 46. , Center Spec. Pub., Berkeley Geochron, No. 2 Maniar, P.D., Piccoli, P.M., Tectonic discrimination of granitoids (1989) Geol. Soc. Am. Bull., 101, pp. 635-643 McReath, I., Lafon, J.M., Davison, I., Chaves, J.M., Conceição, H., Brasiliano-age granitoids in the Sergipana fold Belt, NE Brazil: the coronel João Sá Pluton (1998) J.South Am. Earth Sci., 11, pp. 51-66 Nascimento, R.S., (2005) Domínio Canindé, Faixa Sergipana, nordeste do Brasil: um estudo geoquímico e isotópico de uma seqüência de rifte continental neoproterozóica, p. 140. , Tese de Doutorado, Instituto de Geociências, Universidade Estadual de Campinas Nelson, K.D., Zhao, W., Brow, D.L., Partially molten middle crust beneath southern Tibet, synthesis of Project INDEPTH results (1996) Science, 274, pp. 1684-1688 Neves, S.P., Mariano, G., High-K calc-alcalic plutons in northeast Brazil: origin of biotite diorite/quartz monzonite to granite association and implications for the evolution of the Borborema Province (1997) Int. Geol. Rev., 39, pp. 621-638 Njanko, T., Nédélec, A., Affaton, P., Synkinematic high-K calc-alkaline plutons associated with the Pan-African Central Cameroon shear zone (W-Tibati area): petrology and geodynamic significance (2006) J.Afr. Earth Sci., 44, pp. 494-510 Oliveira, E.P., Carvalho, M.J., Nascimento, R.S., Araújo, M.N.C., Dantas, E., Basilici, G., Bueno, J.F., McNaughton, N., Evidence from detrital zircon geochronology and whole-rock Sm-Nd isotopes for off-craton provenance of clastic metasedimentary units of the Sergipano belt, NE Brazil (2005) XSimpósio Nacional de Estudos TectÔnicos, Curitiba, Paraná, pp. 308-311. , Boletim de Resumos Expandidos Oliveira, E.P., Tarney, J., Petrogenesis of the Canindé de São Francisco complex: a major late Proterozoic gabbroic body in the Sergipe Foldbelt, northeastern Brazil (1990) J.South Am. Earth Sci., 3, pp. 125-140 Oliveira, E.P., Toteu, S.F., Araújo, M.N.C., Carvalho, M.J., Nascimento, R.S., Bueno, J.F., McNaughton, N., Basilici, G., Geologic correlation between the Neoproterozoic Sergipano belt (NE Brazil) and the Yaoundé belt (Cameroon, Africa) (2006) J.Afr. Earth Sci., 44, pp. 470-478 Oliveira, E.P., Windley, B.F., Araújo, M.N.C., The Neoproterozoic Sergipano orogenic belt, NE Brazil: a complete plate tectonic cycle in western Gondwana (2010) Precambrian Res., 181, pp. 64-84 Pearce, J.A., Sources and settings of granitic rocks (1996) Episodes, 19, pp. 120-125 Pearce, J.A., Harris, N.B.W., Tindle, A.G., Trace elements discrimination diagrams for the tectonic interpretation of granitic rocks (1984) J.Petrol., 25, pp. 956-983 Poma, S., Quenardelle, S., Litvak, V., Maisonnave, E.B., Koukharsky, M., The Sierra de Macon, plutonic expression of the Ordovician magmatic arc, Salta Province Argentina (2004) J.South Am. Earth Sci., 16, pp. 587-597 Rickwood, P.C., Boundary lines within petrologic diagrams which use oxides of major and minor elements (1989) Lithos, 22, pp. 247-264 Roberts, M.P., Clemens, J.D., The origin of high-K, calc alkaline, I-type granitoid magmas (1993) Geology, 21, pp. 825-828 Santos, E.J., Van Schmus, W.R., Kozuch, M., Brito Neves, B.B., The Cariris Velhos tectonic event in Northeast Brazil (2010) J.South Am. Earth Sci., 29, pp. 61-76 Santos, R.A., Menezes Filho, N.R., Souza, J.D., Programa Levantamentos Básicos (1988) carta geológica, carta metalogenética e previsional, 4. , 1:100.000, Projeto Carira. DNPM/CPRM,vols Santos, T.J.S., Fetter, A.H., Hackspacher, P.C., Van Schmus, W.R., Nogueira Neto, J.A., Neoproterozoic tectonic and magmatic episodes in the NW sector of the Borborema Province, NE Brazil, during assembly of western Gondwana (2008) J. South Am. Earth Sci., 25, pp. 271-284 Searle, M.P., Simpson, R.L., Law, R.D., Parrish, R.R., Waters, D.J., The structural geometry, metamorphic and magmatic evolution of the Everest massif, High Himalaya of Nepal-South Tibet (2003) J.Geol. Soc., 160, pp. 345-366 Searle, M.P., Szulc, A.G., Channel flow and ductile extrusion of the high Himalayan slab-the Kangchenjunga-Darjeeling profile, Sikkim Himalayaq (2005) J.Asian Earth Sci., 25, pp. 173-185 Silva Filho, A.F., Guimarães, I.P., Lyra de Brito, M.F., Pimentel, M.M., Geochemical signatures of main Neoproterozoic late-tectonic granitoids from the Proterozoic Sergipano Belt, Brazil: significance for the Brasiliano orogeny (1997) Int. Geol. Rev., 39, pp. 639-659 Silva Filho, A.F., Guimarães, I.P., Van Schumus, W.R., Crustal evolution of the Pernambuco-Alagoas Complex, Borborema Province, NE-Brazil: Nd isotopic data from neoproterozoic granitoids (2002) Gondwana Res., 5, pp. 409-422 Silva Filho, A.F., Van Schmus, W.R., Guimarães, I.P., High-K calc-alkaline granitoids of ca. 1 Ga TDM along the limit PE-AL massif/Sergipano Fold Belt, NE Brazil and their geotectonic significance (2000) Rev. Bras. Geociências, 30, pp. 182-185 Smith, J.B., Barley, M.E., Groves, D.I., Krapez, B., Bickle, M.J., Chapman, H.J., The Sholl Shear zone, West Pilbara: evidence for a terrene boundary from integrated tectonics analyses, SHRIMP, U-Pb age-dating and granitoid geochemistry (1998) Precambrian Res., 88, pp. 143-171 Sun, S.-S., McDonough, W.F., Chemical and isotope systematics of oceanic basalts: implications for mantle composition and processes (1989) Magmatism in the Ocean Basins, 42, pp. 313-345. , Geological Society, London, Special Publications Swain, G., Barovich, K., Hand, M., Ferris, G., Schwarz, M., Petrogenesis of the St Peter Suite, southern Australia, Arc magmatism and Proterozoic crustal growth of the South Australian Craton (2008) Precambrian Res., 166, pp. 283-296 Van Schmus, W.R., Brito Neves, B., Hackspacher, P., Babinski, M., U/Pb and Sm/Nd geochronologic studies of the Eastern Borborema Province, Northeastern Brazil: Initial conclusions (1995) J.South Am. Earth Sci., 8, pp. 267-288 Van Schmus, W.R., Kozuch, M., Brito Neves, B.B., Precambrian history of the Zona Transversal of the Borborema Province, NE Brazil: insights from Sm-Nd and U-Pb geochronology (2011) J.South Am. Earth Sci., 31, pp. 227-252 Wang, K.L., Chung, S.L., O'Reilly, S.Y., Sun, S.S., Shinjo, R., Chen, C.H., Geochemical constraints for the genesis of post-collisional magmatism and the geodynamic evolution of the northern Taiwan region (2004) J.Petrol., 45, pp. 975-1011 Whalen, J.B., Percival, J.A., McNicoll, V.J., Geochemical and isotopic (Nd-O) evidence bearing on the origin of late- to post-orogenic high-K granitoid rocks in the Western Superior Province: implications for late Archean tectonomagmatic processes (2004) Precambrian Res., 132, pp. 303-326 Winter, J.D., (2001) An Introduction to Igneous and Metamorphic Petrology, , Prentice Hall