Syn-collisional pan-African granite in the northern part Birnin Gwari schist belt in NW Nigeria
-
2020-09-30 https://doi.org/10.14419/ijag.v8i2.31095 -
Birnin Gwari, Calc-Alkaline, Granite, Nigeria, Quartzolite. -
Abstract
Syn-collisional granite in the northern part of the Birnin Gwari schist belt consists dominantly of granite and lesser granodiorite and quartzolite. Petrographic and ge¬ochemical data revealed three granite groups: the biotite-hornblende granite (quartzolite - BHG); the biotite granite (BG) and the biotite-muscovite granite (BMG). The rocks generally have calc-alkaline and high-K calc-alkaline affinities, and calc-alkalic to alkali-calcic, peraluminous and ferroan and magnesian geochemistry. They are characterized by LILE enrichment, high LREE fractionation factor [(La/Yb) (6.74 to 45.14] with weak to moderate negative Eu (Eu/Eu* = 0.38 to 0.62) and strong negative Nb, P and Ti anomalies. Variation in the behavior of lithophile elements (Ba, Sr and Rb) revealed diverse granite trend such as “high and low Ba-Srâ€; “normalâ€, “anomalous†“strongly differentiated†and “granodiorite and quartz diorite†granite. Their display of similar trace elements and REE patterns suggest they are cogenetic. Major and trace element data indicate differentiation of a mafic magma and partial melting of crustal components inherited from shale-greywacke and quartzose sedimentary protoliths in volcanic arc and post collisional settings. The field and geochemical characteristics of this granite suggest that they are similar to other granites in schist belts in other parts of Nigeria, forming the lateral continuation of the same Pan-African magmatic belt.
Â
Â
Â
-
References
[1] Ajaji, T., Weis, D., Giret, A. and Bouabdellah, M. (1998). Coeval potassic and sodic calc-alkaline series in the post-collisional Hercynian Tanncherfi intrusive complex, Northeastern Morrocco: geochemical, isotopic and geochronological evidence. Lithos 45, 371-393. https://doi.org/10.1016/S0024-4937(98)00040-1.
[2] Ajibade A. C., Anyanwu, N. P. C., Okoro, A. U. and Nwajide, C. S. (2008). The Geology of Minna area. Nigeria Geological Survey Agency Bulletin No 43.
[3] Agunleti, Y. S., Najime, T., Ibrahim, A. A. and Magaji, S. S. (2020). Geology and petrographic studies of rocks in Anka sheet 52, Northwestern Nigeria. Journal of Environmental and Earth Sciences. 10, 53-66.
[4] Akinola, O. O., Talabi, A. O. and Muhammad, H. R. (2017). Petrostructural Features of Metaconglomerate in Igarra and Otuo, South-Western Nigeria. Asian Journal of Earth Sciences, 10, 33-43. https://doi.org/10.3923/ajes.2017.33.43.
[5] Baginski, B., Duchesne, J., Martin, H. and Wiszniewska, J., (2007). Isotopic and geochemical constraints on the evolution of the Mazury granitoids, NE Poland. AM Monogragh No. 1, 11 30.
[6] Batchelor, R. A, Bowden, P. (1985): Petrogenetic interpretation of granitoid rock series using multicationic parameters. Journal of Chemical Geology 48, 43–55 https://doi.org/10.1016/0009-2541(85)90034-8.
[7] Boynton W.V. 1984. Cosmochemistry of the rare earth elements; meteorite studies. In: Henderson P. (Ed.). Rare Earth element geochemistry. Amsterdam: Elsevier. 63-114. https://doi.org/10.1016/B978-0-444-42148-7.50008-3.
[8] Chappell, B.W and White, A.J.R. (1974): Two contrasting granite types. Pacific journal geology.8: pp. 173-174.
[9] Chappell B. W. and Stephens W. E. (1974). Origin of infracrustal (I-type) granite magmas. Transactions of the Royal Society of Edinburgh: Earth Sciences 79, 71-86. https://doi.org/10.1017/S0263593300014139.
[10] Chappell B. W. Bryant, C. J., Wyborn, D., White A. J. R and Williams I. S. 1998. High- and low-temperature I-type granites. Resource Geology 48, 225-226. https://doi.org/10.1111/j.1751-3928.1998.tb00020.x.
[11] Cocherie, A. 1986. Systematic Use of Trace Element Distribution on Patterns in Log-Log Diagrams for Plutonic Suites. Geochimica et Cosmoshimica Acta, 50, 2517-2522. https://doi.org/10.1016/0016-7037(86)90034-7.
[12] Cox, K. G., Bell, J. D., Pankhurst, R. J., (1979). The interpretation of igneous rocks, George, Allen and Unwin, London. https://doi.org/10.1007/978-94-017-3373-1.
[13] Cullers R. L., Podkovyrov V. L., (2002). The source and origin of terrigenous sedimentary rocks in the Mesoproterozoic Ui group, Southeastern Russia. Precambrian Research. 117(3):157–183. https://doi.org/10.1016/S0301-9268(02)00079-7.
[14] Dada, S. S. 1998. Crust-forming ages and Proterozoic crustal evolution in Nigeria: of current interpretations. Precambrian Research 87, 65-74. https://doi.org/10.1016/S0301-9268(97)00054-5.
[15] Dada, S.S., Lancelot, J.R., Briqueu, L., 1989. Age and origin of the annular charnockitic complex at Toro, Northern Nigeria: U--Pb and RbSr evidence. Journal of African Earth Sciences, 9, pp. 227-234. https://doi.org/10.1016/0899-5362(89)90066-3.
[16] Dada, S. S., Birck, J. L., Lancelot, J. R. and Rahaman, M. A. (1993): Archean migmatite-gnesis complex of North Central Nigeria: its geochemistry, Petrogenesis and crustal evolution. In: 16th International Colloquium on African Geology, Mbabane, Swaziland, Extended Abstracts, 1: pp. 97–102.
[17] Danbatta. U. A. 2002. Rb-Sr Isochron Dating of Granitoids from the Kazaure Schist Belt, NW Nigeria. Global Journal of Pure and Applied Sciences 8 (3). 319-322. https://doi.org/10.4314/gjpas.v8i3.16015.
[18] Danbatta. U. A. 2010. On the evolution of Kazaure Schist Belt of NW Nigeria. Global Journal of Geological Sciences 8 (2). 207-216. https://doi.org/10.4314/gjgs.v8i2.62775.
[19] Ekwueme, B.N. and Kroner, A., 1998. Single zircon evaporation ages from the Oban Massif, southeastern Nigeria. Journal of African Earth Sciences, 26, 195 - 205. https://doi.org/10.1016/S0899-5362(98)00005-0.
[20] Ekwueme, B.N. and Pidgeon, R.T. (2001). The Oldest Rocks in West Africa: SHRIMP Zircon Age for Early Achean Migmatitic Orthogneiss at Kaduna, Northern Nigeria. Journal of Geology, university of Chicago,109, 399-406. https://doi.org/10.1086/319979.
[21] El Bouseily, A. M and El-Sokkary, A. A., 1975. The relationship between Rb, Sr and Ba in granitic rocks. Chemical Geology. 16, 174-189. https://doi.org/10.1016/0009-2541(75)90029-7.
[22] Egbuniwe, I., Fitches, W., Bently, M., and Snelling L., 1985. Late Pan-African syenite-granite plutons from NW Nigeria. Journal of African Earth Sciences, 9, 227-234.
[23] Ezepue, M. C and Odigi, M. I., 1993. Petrology and geochemistry of monzodiorite, granodiorite and granites from the Precambrian terrain between Kabba and Lokoja, SW Nig. Jour. Min. Geol; 30, (1): 1-9.
[24] Ferre, E. C., Caby, R., Peucat, J. J., Capdevila, I. R., and Monie, P., 1998. Pan-African post-collisional, ferro-potassic granite and quartz-monzonite plutons of Eastern Nigeria. Lithos, 45, pp. 255 278. https://doi.org/10.1016/S0024-4937(98)00035-8.
[25] Fitches, W.R., Ajibade A. C., Egbuniwe I.G., Holt R. W., and Wright J.B. (1985): Late Proterozoic Schist Belts and Plutonism in NW Nigeria‟, Geological Society of London, 142: pp. 319- 337. https://doi.org/10.1144/gsjgs.142.2.0319.
[26] Garba, I. 2002. Late Pan-African tectonics and origin of Gold mineralization and Rare-metal pegmatites in the Kushaka schist belt, northwestern Nigeria. Journal of Mining and Geology. 38, 1, 1-12. https://doi.org/10.4314/jmg.v38i1.18768.
[27] Girei, M. B. 2015. Geology, geochemistry and petrogenesis of granite suites and pegmatites in the northern part of Mandara Hills Gwoza Sheet 114, Northeastern Nigeria. Unpublished M. Sc. Thesis, Ahmadu Bello University, Zaris.
[28] Goodenough, K. M., Lusty, P. A. J., Roberts, N. M. W., Key, R. M. and Garba, A. 2014. Post-collisional Pan-African granitoids and rare metal pegmatites in western Nigeria: Age, petrogenesis, and the ‘pegmatite conundrum’. Lithos 200, 22-34 https://doi.org/10.1016/j.lithos.2014.04.006.
[29] Grant, N. K. 1978. Structural distinction between metasedimentary cover and an underlying basement in the 600 m.y. old Pan-African domain of Northwestern Nigeria, West African. Geological Society America Bulletin 89, 50-58. https://doi.org/10.1130/0016-7606(1978)89<50:SDBAMC>2.0.CO;2.
[30] Grigoriev, S. I. and Pshenichny, C. A., 1998. Late Mesozoic post-collisional intermediate to silicic magmatism in the Badjal area, far east of Russia. Lithos 45, 457-468. Kröner, A., Hassanen M.A., El-nisr S.A., and Mohamed F.H (1996): Geochemistry and petrogenesis of Pan-African I-type granitoids at Gabal Igla Ahmar, Eastern Desert, Egypt. Journal of African Earth Science 22, (1): pp. 29-42 https://doi.org/10.1016/S0024-4937(98)00044-9.
[31] Harris, N. B. W., Pearce, J. A. and Tindle, A. G., 1986. Geochemical characteristics of collision-zone magmatism. In: Coward, M. P. and Reis, A. C. (eds.) Collision tectonics. Special Publication of the Geological Society, 19, pp. 67 -81. https://doi.org/10.1144/GSL.SP.1986.019.01.04.
[32] Igonoh, E. E., and Abimbola, A. F. 1971. Geochemistry of Pan-African Granitoids, Southwest Nigeria: Evidence of Magmatic Mixing, Journal of Geography, Environment and Earth Science International 5(4): 1-17 https://doi.org/10.9734/JGEESI/2016/19041.
[33] Irvine, T. N., and Baragar, W. R. A. 1971. A Guide to the Chemical Classification of Common Volcanic Rocks. Canadian Journal of Earth Sciences, 8, (5), 523-548. https://doi.org/10.1139/e71-055.
[34] Karacik, Z., Yilmaz, Y., Pearce, J. A. and Ece, O. I., 2008. Petrochemistry of the south Marmara granitoids, northwest Anatolia, Turkey. International Journal of Earth Sciences (Geol Rundsch), 97, pp. 1191-1200. https://doi.org/10.1007/s00531-007-0222-y.
[35] Lissan, H. N., Bakheit, A. K.., 2011. Geochemistry and geotectonic setting of Neoproterozoic Granitoids from Artoli Area, Berber Province Northern Sudan. Journal of Applied Sciences. 11 (5), 752-767. https://doi.org/10.3923/jas.2011.752.767.
[36] Makanjuola, A.A. 1982. A Review of the Petrology of the Nigerian syenites. Journal of Mining and Geology, 19(2), 1 14.
[37] Maniar, P. D. and Piccoli, P. M., 1989. Tectonic discrimination of granitoids. Geological Society of American Bulletin, 101, pp. 635 -643. https://doi.org/10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2.
[38] McCurry, P. 1976. The geology of the Precambrian to Lower Palaeozoic of northern Nigeria- a review. In: Geology of Nigeria. C.A. Kogbe (Ed). Elizabethan Publishing Company. Lagos, 15-39.
[39] Miyashiro A (1978). Nature of alkalic volcanic rock series. Contrib. Mineral Petrol. 66: 91–104.
[40] Obiora, S. C., 2006. Petrology and Geotectonic Setting of B asement Complex Rocks around Ogoja, Southeastern Nigeria. Ghana Journal of Science, 46, pp. 13 - 25. https://doi.org/10.4314/gjs.v46i1.15912.
[41] Obiora, S. C. (1986): Chemical characterization and tectonic evolution of hornblende-biotite granitoids from the Precambrian Basement Complex around Itowanye and Katsina-Ala, southeastern Nigeria. Journal of Mining and Geology Vol. 48(1): pp. 13-29.
[42] O‟Connor, J. T. (1965). A classification for quartz-rich igneous rocks based on feldspar ratios. US Geological Survey, Professional Papers 52(5): pp. 79-84.
[43] Odewumi, S. C., Olarewaju, V. O. (2013) Petrogenesis and Geotectonic Settings of the Granitic Rocks of Idofin-osi-eruku Area, Southwestern Nigeria using Trace Element and Rare Earth Element Geochemistry. Journal of Geology and Geosciences 2: 109. https://doi.org/10.4172/2329-6755.1000109.
[44] Okonkwo, C. T. and Winchester, J. A., 2004. Geochemistry of granitic rocks in Jebba area, southwestern Nigeria. Journal of Mining and Geology, Vol. 40(2), pp. 95 - 100. https://doi.org/10.4314/jmg.v40i2.18814.
[45] Oluyede, O. K., Garba, I., Danbatta, U., Ogunleye, P. and Klötzli, U. (2020). Field occurrence, petrography and structural characteristics of basement rocks of the northern part of Kushaka and Birnin Gwari schist belts, northwestern Nigeria. Journal of Natural Sciences Research. ISSN (Paper) 2224-3186 (Online) 2225-0921 https://doi.org/10.7176/JNSR.
[46] Oluyede, O. K., Garba, I., Danbatta, U., Ogunleye, P. and Klötzli, U. (2020). Geochemistry and petrogenesis of banded and granitic gneisses of the northern part of Kushaka schist belts northwestern Nigeria. Journal of Environmental and Earth Science. ISSN (Paper) 2224-3216 (Online) 2225-0948 https://doi.org/10.7176/JEES.
[47] Onyeagocha A. C. (1986): Geochemistry of basement granitic rocks from northcentral Nigeria. Journal of African Earth Science 5(2): pp. 651-657. https://doi.org/10.1016/0899-5362(86)90032-1.
[48] Oyawoye, M.O., 1972. The Basement Complex of Nigeria in Dessauvagie, T.F.J. and Whiteman, A.J. (eds). African Geology. Ibadan University Press, Ibadan, pp. 67 -99.
[49] Oyinloye, A. O. and Ojo, A. O. (1988). Physical and Mineral Evaluation of lay Deposits at Ado-Ekiti. Journal of Techno-Science, (2) 1 Pg 49-52.
[50] Olarewaju, V. O. (1988). “Petrology and geochemistry of the charnockitic and associated granitic rocks of Ado-Ekiti, Akure, S.W. Nigeriaâ€. In: Precambian Geology of Nigeria. pp 231-239. Geological Survey of Nigeria Publication.
[51] Olarewaju, V. O. and Rahaman, M. A., 1982. Petrology and Geochemistry of Older Granites from some parts of Northern Nigeria. Journal of Mining and Geology, 18(2), pp. 16-28.
[52] Pearce, J. A. Harris, N. B. W. and Tindle, A. G. W. 1984. Trace Element Discrimination Diagrams for the Tectonic Ä°nterpretation of Granitic Rocks. Journal of Petrology, 25, (4), 956-983. https://doi.org/10.1093/petrology/25.4.956.
[53] Peccerillo, A., and Taylor, S. R. (1976): Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contributions to Mineralogy and Petrology, 58: pp. 63-81. https://doi.org/10.1007/BF00384745.
[54] Rahaman, M. A. 1976. Review of the basement geology of southwestern Nigeria. In: Geology of Nigeria. (Edited by C. A. Kogbe). Elizabethan Publishing Company Lagos, 41-58
[55] Rahaman, M. A. 1988. Recent advances in the study of the basement complex of Nigeria. In: Precambrian Geology of Nigeria. (Eds. Oluyide et al.) a publication of the Geological Survey Nigeria. 71-43.
[56] Roberts, M. P. and Clemens J. D. 1993. The origin of high-potassium calc-alkaline I-type granitoids. Geology 21, 825-828. https://doi.org/10.1130/0091-7613(1993)021<0825:OOHPTA>2.3.CO;2.
[57] Roddaz M, Viers J, Brusset S, Baby P, Boucayrand C, Hérail G. (2006). Controls on weathering and provenance in the Amazonian foreland basin: Insights from major and trace element geochemistry of Neogene Amazonian sediments. Chemical Geology. 226 (1) 31-65. https://doi.org/10.1016/j.chemgeo.2005.08.010.
[58] Rollinson, H. R., 1993. Using Geochemical Data: Evaluation, Presentation and Interpretation. Longman Group, Uk Ltd. Co-published in the United States with John Wiley and Sons, New York, 352.
[59] Rottura, A., Bargossi, G. M., Caggianeli, A., Del Moro, A., Visona, D. and Tranne, C. A. 1998. Origin and significance of the Permian high-K calc-alkaline magmatism in the central-eastern Southern Alps, Italy. Lithos 45, (1-4) 329-348. https://doi.org/10.1016/S0024-4937(98)00038-3.
[60] Russ, W. 1957. The geology of parts of Niger, Zaria and Sokoto provinces with reference to the occurrence of gold. Geological Survey Nigeria Bulletin 29.
[61] Schluter, T., 2005. Geological Atlas of Africa: With Notes on Stratigraphy, Tectonics, Economic Geology, Geohazards, Geosites and Geoscientific Education of Each Country. 2nd Edition. Springer, 272p.
[62] Streckeisen, A., (1976). To each plutonic rock its proper name. Earth Science Review 6: 181-217.
[63] Sun S. S. and McDonough, W. F. (1989). Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunders A.D., Norry M.J. (Eds.). Magmatism in the ocean basins. Geological Society of London, Special Publication, 42:313-345. https://doi.org/10.1144/GSL.SP.1989.042.01.19.
[64] Sun, L. M. and Chen, J. C. (1992) Geochemical study of granites from Chimen (Quemoy) and Hong Kong, Southeastern China. Journal of Southeast Asian Earth Sciences 7, (4), 237-245. https://doi.org/10.1016/0743-9547(92)90003-T.
[65] Tarney J. & Jones C.E. 1994. Trace element geochemistry of orogenic igneous rocks and crustal growth models. Journal of the Geological Society, 151(5):855-868. https://doi.org/10.1144/gsjgs.151.5.0855.
[66] Thiéblemont and Tegyey, (1994). D. Thiéblemont and M. Tegyey, Une discrimination géochimique des roches différenciées témoin de la diversité d’origine et de situation tectonique des magmas calco-alcalins, Comptes Rendus de l’Académie des Sciences Paris 319 (1994), pp. 87–94.
[67] Tubosun, I. A., Lancelot, J. R., Rahaman, M. A., Ocan, O., 1984. U–Pb Pan-African ages of two charnockite-granite association from southwestern Nigeria. Contribution to Mineralogy and Petrology 88, 188–195. https://doi.org/10.1007/BF00371422.
[68] Turner, D. C. 1983: Upper Proterozoic schist belts in the Nigerian sector of the Pan African Province of West Africa. Precambrian Research 21, 5-79. https://doi.org/10.1016/0301-9268(83)90005-0.
[69] Ukwang, E., and Ekwueme, B. N. (2009): Geochemistry and geotectonic study of granitic rocks of southwest Obudu Plateau, southeastern Nigeria. Journal of Mining and Geology, 45: pp. 73-82.
[70] Van Breemen, O., Pidgeon, R. T. and Bowden, P. 1977. Age and isotopic studies of some Pan-African granites from North-central Nigeria. Precambrian Research 4, 319-407. https://doi.org/10.1016/0301-9268(77)90001-8.
[71] Whalen J. B., Currie K. L. and Chappell B. W. 1987. A-type granites: Geochemical characteristics, discrimination and petrogenesis. Contributions Mineralogy Petrology 95: 407-419. https://doi.org/10.1007/BF00402202.
[72] White, A. J. R., (2001) Water, Restite and Granite Mineralization. Australian Journal of Earth Sciences, 48, 551-555. https://doi.org/10.1046/j.1440-0952.2001.00878.x.
[73] Zorano S. S; Martin H., Jean-jacques P; Emanuel F. J. and Maria H. F. M. (2007): Calc-Alkaline Magmatism at the Archean-Proterozoic Transition: the Caico Basement Complex (NE Brazil) Journal of Petrology 48 (11): pp. 2149-2185 https://doi.org/10.1093/petrology/egm055.
-
Downloads
-
How to Cite
Oluyede, K., & Klötzli, U. (2020). Syn-collisional pan-African granite in the northern part Birnin Gwari schist belt in NW Nigeria. International Journal of Advanced Geosciences, 8(2), 197-213. https://doi.org/10.14419/ijag.v8i2.31095Received date: 2020-08-19
Accepted date: 2020-09-17
Published date: 2020-09-30