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Sedimentary provenance and maximum depositional age analysis of the Cretaceous? Lapur and Muruanachok sandstones (Turkana Grits), Turkana Basin, Kenya

Published online by Cambridge University Press:  03 December 2018

Prince C. Owusu Agyemang*
Affiliation:
Geosciences, College of Science and Engineering, James Cook University, Townsville, QLD 4811, Australia
Eric M. Roberts
Affiliation:
Geosciences, College of Science and Engineering, James Cook University, Townsville, QLD 4811, Australia
Bob Downie
Affiliation:
Bowleven plc, 2nd Floor West, Rosebery House, 9 Haymarket Terrace, Edinburgh EH12 5EZ, UK
Joseph J. W. Sertich
Affiliation:
Department of Earth Sciences, Denver Museum of Nature & Science, Denver, Colorado, USA
*
Author for correspondence: Prince C. Owusu Agyemang, Email: princecharles.owusuagyemang@my.jcu.edu.au

Abstract

The Turkana Basin of northwestern Kenya is well known for its rich Neogene–Quaternary vertebrate fossil record; however, it also represents one of the few locations in sub-Saharan Africa where Cretaceous vertebrate fossils, including dinosaurs and other archosaurs, are preserved. These Cretaceous deposits are colloquially referred to as the ‘Turkana Grits’, and assumed to be Cretaceous in age based on their limited biostratigraphy. The ‘Turkana Grits’ are overlain by Palaeogene volcanic rocks (<35 Ma), which are widely considered to record the earliest evidence of plume-related volcanism in the East African Rift System. In this study, we present the results of an integrated sedimentary provenance investigation of two units within the ‘Turkana Grits’ called the Lapur and Muruanachok sandstones. Analysis of U–Pb ages and Lu–Hf initial ɛHf(t) values from 1106 detrital zircons demonstrate that sediments are primarily derived from Neoarchaean and Neoproterozoic basement sources, except for six Palaeogene grains from the upper Lapur Sandstone, which are of unknown provenance. Considered together, these data point to the Mozambique Belt, which makes up the nearby rift flanks, as the primary provenance source. This is consistent with palaeocurrent data, and suggests localized sediment input by alluvial fans, which fed into NNW-directed fluvial systems. Perhaps the most surprising finding is the identification of the late Paleocene detrital zircons, which not only demonstrate that the depositional age for the top of the formation is Paleocene rather than Cretaceous, but also provides possible evidence for the oldest Palaeogene volcanic activity within the East African Rift System.

Type
Original Article
Copyright
© Cambridge University Press 2018 

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References

Aleinikoff, JN, Schenck, WS, Plank, MO, Srogi, L, Fanning, CM, Kamo, SL and Bosbyshell, H (2006) Deciphering igneous and metamorphic events in high-grade rocks of the Wilmington complex, Delaware: morphology, cathodoluminescence and backscattered electron zoning, and SHRIMP U–Pb geochronology of zircon and monazite. Geological Society of America Bulletin 118, 3964.CrossRefGoogle Scholar
Amiot, R, Buffetaut, E, Lécuyer, C, Wang, X, Boudad, L, Ding, Z, Fourel, F, Hutt, S, Martineau, F, Medeiros, MA and Mo, J (2010) Oxygen isotope evidence for semi-aquatic habits among spinosaurid theropods. Geology 38, 139–42.CrossRefGoogle Scholar
Arambourg, C (1935) Esquisse géologique de la bordure occidentale du Lac Rodolphe. In Mission Scientifique de l’Omo, 1932–1933, Vol. 1, Fasc. 1, pp. 916. Paris: Muséum National d’Histoire Naturelle.Google Scholar
Arambourg, C (1943) Contribution a l’etude geologique et paleontologique du Bassin du Lac Rodolphe et de la Basse Vallee de l’Omo. In Mission Scientifique de l’Omo, 1932–1933, Vol. 1, Fasc. 2, pp. 157230. Paris: Muséum National d’Histoire Naturelle.Google Scholar
Arambourg, C and Wolff, RG (1969) Nouvelles donnees paleontologique sur l’age des “gres du Lubur” (Turkana Grits) a l’Ouest du lac Rudolphe. Compte Rendu Sommaire des Séances de la Société Géologique de France 6, 190202.Google Scholar
Averianov, A (2014) Review of taxonomy, geographic distribution, and paleoenvironments of Azhdarchidae (Pterosauria). ZooKeys 432, 1107.CrossRefGoogle Scholar
Baker, BH, Mohr, PA and Williams, LAJ (1972) Geology of the eastern rift system of Africa. Geological Society of America Special Papers 136, 168.CrossRefGoogle Scholar
Barth, H and Meinhold, KD (1979) Mineral prospecting in the Bayuda Desert. Technical Report of the Sudanese–German Exploration Project, Vol. A. Hannover: BGR.Google Scholar
Batumike, JM, Griffin, WL, O’Reilly, SY, Belousova, EA and Pawlitschek, M (2009) Crustal evolution in the central Congo-Kasai Craton, Luebo, DR Congo: insights from zircon U–Pb ages, Hf-isotope and trace-element data. Precambrian Research 170, 107–15.CrossRefGoogle Scholar
Bauer, FU, Karl, M, Glasmacher, UA, Nagudi, B, Schumann, A and Mroszewski, L (2012) The Rwenzori Mountains of western Uganda – aspects on the evolution of their remarkable morphology within the Albertine Rift. Journal of African Earth Sciences 73, 4456.CrossRefGoogle Scholar
Begg, GC, Griffin, WL, Natapov, LM, O’Reilly, SY, Grand, SP, O’Neill, CJ, Hronsky, JMA, Poudjom, Djomani Y, Swain, CJ, Deen, T and Bowden, P (2009) The lithospheric architecture of Africa: seismic tomography, mantle petrology, and tectonic evolution. Geosphere 5, 2350.CrossRefGoogle Scholar
Bellieni, G, Visentin, EJ, Zanettin, B, Piccirillo, EM, Di Brozolo, F and Rita, F (1981) Oligocene transitional-tholeiitic magmatism in northern Turkana (Kenya). Comparison with the coeval Ethiopian volcanism. Bulletin of Volcanology 44, 411–27.CrossRefGoogle Scholar
Belousova, E, Griffin, WL, O’Reilly, SY and Fisher, NL (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology 143, 602–22.CrossRefGoogle Scholar
Benkhelil, J (1989) The origin and evolution of the Cretaceous Benue Trough (Nigeria). Journal of African Earth Sciences (and the Middle East) 8, 251–82.CrossRefGoogle Scholar
Bertrand, H, Féraud, G and Mascle, J (1993) Alkaline volcano of Paleocene age on the Southern Guinean Margin: mapping, petrology, 40Ar–39Ar laser probe dating, and implications for the evolution of the Eastern Equatorial Atlantic. Marine Geology 114, 251–62.CrossRefGoogle Scholar
Black, LP, Kamo, SL, Allen, CM, Aleinikoff, JN, Davis, DW, Korsch, RJ and Foudoulis, C (2003) TEMORA 1: a new zircon standard for Phanerozoic U–Pb geochronology. Chemical Geology 200, 155–70.CrossRefGoogle Scholar
Boschetto, H, Brown, FH and McDougall, IM (1992) Stratigraphy of the Lothidok Range, northern Kenya, and K/Ar ages of its Miocene primates. Journal of Human Evolution 22, 4771.CrossRefGoogle Scholar
Bosworth, W (1992) Mesozoic and early Tertiary rift tectonics in East Africa. Tectonophysics 209, 115–37.CrossRefGoogle Scholar
Bosworth, W (2015) Geological evolution of the Red Sea: historical background, review, and synthesis. In The Red Sea (pp. 4578). Berlin, Heidelberg: Springer.Google Scholar
Bosworth, W and Morley, CK (1994) Structural and stratigraphic evolution of the Anza Rift, Kenya. Tectonophysics 236, 93115.CrossRefGoogle Scholar
Bosworth, W and Stockli, DF (2016) Early magmatism in the greater Red Sea rift: timing and significance. Canadian Journal of Earth Sciences 53, 1158–76.CrossRefGoogle Scholar
Bosworth, W, Stockli, DF and Helgeson, DE (2015) Integrated outcrop, 3D seismic, and geochronologic interpretation of Red Sea dike-related deformation in the Western Desert, Egypt – the role of the 23Ma Cairo “mini-plume”. Journal of African Earth Sciences 109, 107–19.CrossRefGoogle Scholar
Bouvier, A, Vervoort, JD and Patchett, PJ (2008) The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Science Letters 273, 4857.CrossRefGoogle Scholar
Brown, FH and McDougall, I (2011) Geochronology of the Turkana Depression of northern Kenya and southern Ethiopia. Evolutionary Anthropology: Issues, News, and Reviews 20, 217–27.CrossRefGoogle ScholarPubMed
Browne, SE and Fairhead, JD (1983) Gravity study of the Central African Rift System: a model of continental disruption 1. The Ngaoundere and Abu Gabra rifts. Tectonophysics 94, 187203.CrossRefGoogle Scholar
Cahen, L, Snelling, NJ, Delhal, J and Vail, J (1984) The Geochronology and Evolution of Africa. Oxford: Clarendon Press, 512 pp.Google Scholar
Carrapa, B (2010) Resolving tectonic problems by dating detrital minerals. Geology 38, 191–2.CrossRefGoogle Scholar
Cawood, PA, Hawkesworth, CJ and Dhuime, B (2012) Detrital zircon record and tectonic setting. Geology 40, 875–8.CrossRefGoogle Scholar
Chorowicz, J (2005) The East African rift system. Journal of African Earth Sciences 43, 379410.CrossRefGoogle Scholar
Coffin, MF and Rabinowitz, PD (1988) Evolution of the conjugate East African-Madagascan margins and the western Somali Basin. Geological Society of America Special Papers 226, 179.CrossRefGoogle Scholar
Condie, KC, Beyer, E, Belousova, E, Griffin, WL and O’Reilly, SY (2005) U–Pb isotopic ages and Hf isotopic composition of single zircons: the search for juvenile Precambrian continental crust. Precambrian Research 139, 42100.CrossRefGoogle Scholar
Corfu, F and Noble, SR (1992) Genesis of the southern Abitibi greenstone belt, Superior Province, Canada: evidence from zircon Hf isotope analyses using a single filament technique. Geochimica et Cosmochimica Acta 56, 2081–97.CrossRefGoogle Scholar
Cullers, RL, Bock, B and Guidotti, C (1997) Elemental distributions and neodymium isotopic compositions of Silurian metasediments, western Maine, USA: redistribution of the rare earth elements. Geochimica et Cosmochimica Acta 61, 1847–61.CrossRefGoogle Scholar
Cutten, HNC, Johnson, SP and De Waele, B (2006) Tectonic evolution of the Mozambique Belt, Eastern Africa. In 21st Colloquium of African Geology. Maputo, Mozambique. 3–5 July, 2006, Abstract Volume, pp. 33–4.Google Scholar
de Wit, MJ and Linol, B (2015) Precambrian Basement of the Congo Basin and its flanking terrains. In Geology and Resource Potential of the Congo Basin (eds de Wit, M, Guillocheau, F and de Wit, MCJ), pp. 1937. Dordrecht: Springer.Google Scholar
Dhuime, B, Hawkesworth, C and Cawood, P (2011) When continents formed. Science 331, 154–5.CrossRefGoogle ScholarPubMed
Dickinson, WR (1985) Interpreting provenance relations from detrital modes of sandstones. In Provenance of Arenites, pp. 333–61. Netherlands: Springer.CrossRefGoogle Scholar
Dickinson, WR, Beard, LS, Brakenridge, GR, Erjavec, JL, Ferguson, RC, Inman, KF, Lindberg, FA and Ryberg, PT (1983) Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geological Society of America Bulletin 94, 222–35.2.0.CO;2>CrossRefGoogle Scholar
Dickinson, WR and Gehrels, GE (2009) Use of U–Pb ages of detrital zircons to infer maximum depositional ages of strata: a test against a Colorado Plateau Mesozoic database. Earth and Planetary Science Letters 288, 115–25.CrossRefGoogle Scholar
Dickinson, WR and Suczek, CA (1979) Plate tectonics and sandstone compositions. American Association of Petroleum Geologists Bulletin 63, 2164–82.Google Scholar
Ducrocq, S, Boisserie, JR, Tiercelin, JJ, Delmer, C, Garcia, G, Kyalo, MF, Leakey, MG, Marivaux, L, Otero, O, Peigné, S, Tassy, P and Lihoreau, F (2010) New Oligocene vertebrate localities from Northern Kenya (Turkana Basin). Journal of Vertebrate Paleontology 30, 293–9.CrossRefGoogle Scholar
Dunkelman, TJ, Rosendahl, BR and Karson, JA (1989) Structure and stratigraphy of the Turkana Rift from seismic reflection data. Journal of African Earth Sciences (and the Middle East) 8, 489510.CrossRefGoogle Scholar
Ebinger, CJ (1989) Tectonic development of the western branch of the East African rift system. Geological Society of America Bulletin 101, 885903.2.3.CO;2>CrossRefGoogle Scholar
Ebinger, CJ and Ibrahim, A (1994) Multiple episodes of rifting in central and east Africa: a re-evaluation of gravity data. Geologische Rundschau 83, 689702.CrossRefGoogle Scholar
Ebinger, CJ and Sleep, NH (1998) Cenozoic magmatism throughout east Africa resulting from impact of a single plume. Nature 395, 788.CrossRefGoogle Scholar
Emerick, CM and Duncan, RA (1982) Age progressive volcanism in the Comores Archipelago, western Indian Ocean and implications for Somali plate tectonics. Earth and Planetary Science Letters 60, 415–28.CrossRefGoogle Scholar
Feibel, CS (2011) A geological history of the Turkana Basin. Evolutionary Anthropology 20, 206–16.CrossRefGoogle ScholarPubMed
Feibel, CS, Brown, FH and McDougall, I (1989) Stratigraphic context of fossil hominids from the Omo Group deposits: northern Turkana Basin, Kenya and Ethiopia. American Journal of Physical Anthropology 78, 595622.CrossRefGoogle ScholarPubMed
Fisher, CM, Hanchar, JM, Samson, SD, Dhuime, B, Blichert-Toft, J, Vervoort, JD and Lam, R (2011) Synthetic zircon doped with hafnium and rare earth elements: a reference material for in situ hafnium isotope analysis. Chemical Geology 286, 3247.CrossRefGoogle Scholar
Fisher, CM, Vervoort, JD and Hanchar, JM (2014) Guidelines for reporting zircon Hf isotopic data by LA-MC-ICPMS and potential pitfalls in the interpretation of these data. Chemical Geology 363, 125–33.CrossRefGoogle Scholar
Fleagle, J and Leakey, M (2011) The Turkana Basin introduction. Evolutionary Anthropology 20, 201.CrossRefGoogle Scholar
Folk, RL (1980) Petrology of Sedimentary Rocks. Austin, TX: Hemphill Publishing Company.Google Scholar
Fortelius, M, Zliobaite, I, Kaya, F, Bibi, F, Bobe, R, Leakey, L and Werdelin, L (2016) An ecometric analysis of the fossil mammal record of the Turkana Basin. Philosophical Transactions of the Royal Society of London: Biological Sciences 371, 20150232, doi: 10.1098/rstb.2015.0232.CrossRefGoogle ScholarPubMed
Foster, DA, Goscombe, BD, Newstead, B, Mapani, B, Mueller, PA, Gregory, LC and Muvangua, E (2015) U–Pb age and Lu–Hf isotopic data of detrital zircons from the Neoproterozoic Damara Sequence: implications for Congo and Kalahari before Gondwana. Gondwana Research 28, 179–90.CrossRefGoogle Scholar
Francis, PW, Thorpe, RS and Ahmed, F (1973) Setting and significance of Tertiary–Recent volcanism in the Darfur province of western Sudan. Nature 243, 30–2.Google Scholar
Franz, G, Harms, U, Denkler, T and Pasteels, P (1993) Late Cretaceous igneous activity in the Delgo uplift (Northern Province, Sudan). In Geoscientific Research in Northeast Africa (eds Thorweihe, U and Schandelmeier, H), pp. 227–30. Rotterdam: Balkema.Google Scholar
Franz, G, Puchelt, H and Pasteels, P (1987) Petrology, geochemistry and age relations of Triassic and Tertiary volcanic rocks from SW Egypt and NW Sudan. Journal of African Earth Sciences (1983) 6, 335–52.CrossRefGoogle Scholar
Gehrels, GE (2012) Detrital zircon U–Pb geochronology: current methods and new opportunities. In Tectonics of Sedimentary Basins: Recent Advances (eds Busby, C and Azor, A), pp. 4762. Hoboken, NJ: John Wiley & Sons.Google Scholar
Gehrels, GE, Valencia, VA and Ruiz, J (2008) Enhanced precision, accuracy, efficiency, and spatial resolution of U–Pb ages by laser ablation–multicollector–inductively coupled plasma–mass spectrometry. Geochemistry, Geophysics, Geosystems 9, Q03017, doi: 10.1029/2007GC001805.CrossRefGoogle Scholar
Genik, GJ (1993) Petroleum geology of Cretaceous–Tertiary rift basins in Niger, Chad, and Central African Republic. American Association of Petroleum Geologists Bulletin 77, 1405–34.Google Scholar
George, R, Rogers, N and Kelley, S (1998) Earliest magmatism in Ethiopia: evidence for two mantle plumes in one flood basalt province. Geology 26, 923–6.2.3.CO;2>CrossRefGoogle Scholar
Grantham, GH, Maboko, M and Eglington, BM (2003) A review of the evolution of the Mozambique Belt and implications for the amalgamation and dispersal of Rodinia and Gondwana. In Proterozoic East Gondwana: Supercontinent Assembly and Breakup (eds Yoshida, M, Windley, BE and Dasgupta, S), pp. 401–25. Geological Society of London, Special Publication no. 206.Google Scholar
Griffin, W, Belousova, E, Shee, S, Pearson, N and O’Reilly, S (2004) Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons. Precambrian Research 131, 231–82.CrossRefGoogle Scholar
Grimes, CB, John, BE, Kelemen, PB, Mazdab, FK, Wooden, JL, Cheadle, MJ, Hanghoj, K and Schwartz, JJ (2007) Trace element chemistry of zircons from oceanic crust: a method for distinguishing detrital zircon provenance. Geology 35, 643–6.CrossRefGoogle Scholar
Guillong, M, Meier, DL, Allan, MM, Heinrich, CA and Yardley, BW (2008) Appendix A6: SILLS: a MATLAB-based program for the reduction of laser ablation ICP-MS data of homogeneous materials and inclusions. Mineralogical Association of Canada Short Course Series 40, 328–33.Google Scholar
Guynn, J and Gehrels, G (2010) Comparison of Detrital Zircon Age Distributions Using the KS Test Visualization and Representation of Age-Distribution Data Histograms: Tucson. Arizona: Arizona LaserChron Center, University of Arizona, 16 pp.Google Scholar
Harris, NBW, Hawkesworth, CJ and Ries, AC (1984) Crustal evolution in north-east and east Africa from model Nd ages. Nature 309, 773–6.CrossRefGoogle Scholar
Hastings, AK, Bloch, JI and Jaramillo, CA (2011) A new longirostrine dyrosaurid (Crocodylomorpha, Mesoeucrocodylia) from the Paleocene of north-eastern Colombia: biogeographic and behavioural implications for New-World Dyrosauridae. Palaeontology 54, 1095–116.CrossRefGoogle Scholar
Hauzenberger, CA, Sommer, H, Fritz, H, Bauernhofer, A, Kröner, A, Hoinkes, G, Wallbrecher, E and Thöni, M (2007) SHRIMP U–Pb zircon and Sm–Nd garnet ages from the granulite-facies basement of SE Kenya: evidence for Neoproterozoic polycyclic assembly of the Mozambique Belt. Journal of the Geological Society, London 164, 189201.CrossRefGoogle Scholar
Hawkesworth, CJ and Kemp, AIS (2006) Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution. Chemical Geology 226, 144–62.CrossRefGoogle Scholar
Hepworth, JV (1972) The Mozambique orogenic belt and its foreland in northeast Tanzania: a photogeologically-based study. Journal of the Geological Society, London 128, 461–94.CrossRefGoogle Scholar
Hepworth, JV and Kennerley, JB (1969) Photogeology and structure of the Mozambique orogenic front near Kolo, north-east Tanzania. Quarterly Journal of the Geological Society 125, 447–79.CrossRefGoogle Scholar
Holmes, A (1951) The sequence of Precambrian orogenic belts in south and central Africa. In 18th International Geological Congress, London, 1948, Part 14, pp. 254–69.Google Scholar
Hoskin, PWO (2005) Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta 69, 637–48.CrossRefGoogle Scholar
Hoskin, PWO and Ireland, TR (2000) Rare earth element chemistry of zircon and its use as a provenance indicator. Geology 28, 627–30.2.0.CO;2>CrossRefGoogle Scholar
Hoskin, PWO and Schaltegger, U (2003) The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry 53, 2762.CrossRefGoogle Scholar
Ingersoll, RV, Bullard, TF, Ford, RL, Grimm, JP, Pickle, JD and Sares, SW (1984) The effect of grain size on detrital modes: a test of the Gazzi-Dickinson point-counting method. Journal of Sedimentary Research 54, 103–16.Google Scholar
Institut Français du Pétrole. Bureau d’Études Industrielles et de Coopération (1987) Geological Map of Kenya with Bouguer Gravity Contours. Nairobi: Ministry of Energy and Regional Development.Google Scholar
Jackson, SE, Pearson, NJ, Griffin, WL and Belousova, EA (2004) The application of laser ablation-inductively coupled plasma-mass spectrometry to in-situ U–Pb zircon geochronology. Chemical Geology 211, 4769.CrossRefGoogle Scholar
Jacobs, LL, Winkler, DA and Gomani, EM (1996) Cretaceous dinosaurs of Africa: examples from Cameroon and Malawi. Memoirs o the Queensland Museum 39, 595610.Google Scholar
Jian, X, Guan, P, Zhang, DW, Zhang, W, Feng, F, Liu, RJ and Lin, SD (2013) Provenance of Tertiary sandstone in the northern Qaidam basin, northeastern Tibetan Plateau: integration of framework petrography, heavy mineral analysis and mineral chemistry. Sedimentary Geology 290, 109–25.CrossRefGoogle Scholar
Jorge, RCGS, Fernandes, P, Rodrigues, B, Pereira, Z and Oliveira, JT (2013) Geochemistry and provenance of the Carboniferous Baixo Alentejo Flysch Group, South Portuguese Zone. Sedimentary Geology 284, 133–48.CrossRefGoogle Scholar
Jouve, S, Bouya, B and Amaghzaz, M (2008) A long-snouted dyrosaurid (Crocodyliformes, Mesoeucrocodylia) from the Paleocene of Morocco: phylogenetic and palaeobiogeographic implications. Palaeontology 51, 281–94.CrossRefGoogle Scholar
Kabete, JM, McNaughton, NJ, Groves, DI and Mruma, AH (2012) Reconnaissance SHRIMP U–Pb zircon geochronology of the Tanzania Craton: evidence for Neoarchean granitoid–greenstone belts in the Central Tanzania Region and the Southern East African Orogen. Precambrian Research 216, 232–66.CrossRefGoogle Scholar
Kadima, E, Delvaux, D, Sebagenzi, SN, Tack, L and Kabeya, SM (2011) Structure and geological history of the Congo Basin: an integrated interpretation of gravity, magnetic and reflection seismic data. Basin Research 23, 499527.CrossRefGoogle Scholar
Kemp, AIS, Foster, GL, Scherstén, A, Whitehouse, MJ, Darling, J and Storey, C (2009) Concurrent Pb–Hf isotope analysis of zircon by laser ablation multi-collector ICP-MS, with implications for the crustal evolution of Greenland and the Himalayas. Chemical Geology 261, 244–60.CrossRefGoogle Scholar
Key, RM, Charsley, TJ, Hackman, BD, Wilkinson, AT and Rundle, CC (1989) Superimposed upper Proterozoic collision-controlled orogenies in the Mozambique orogenic belt of Kenya. Precambrian Research 44, 197225.CrossRefGoogle Scholar
Kinny, PD and Mass, R (2003) Lu–Hf and Sm–Nd isotope systems in zircon. In Zircon: Reviews in Mineralogy and Geochemistry Vol. 53 (eds Hanchar, JM and Hoskin, PWO), pp. 327–41. Washington, DC: Mineralogical Society of America.CrossRefGoogle Scholar
Kovacs, R, Schlosser, S, Staub, SP, Schmiderer, A, Pernicka, E and Günther, D (2009) Characterization of calibration materials for trace element analysis and fingerprint studies of gold using LA-ICP-MS. Journal of Analytical Atomic Spectrometry 24, 476–83.CrossRefGoogle Scholar
Kröner, A (2001) The Mozambique Belt of East Africa and Madagascar: significance of zircon and Nd model ages for Rodinia and Gondwana supercontinent formation and dispersal. South African Journal of Geology 104, 151–66.CrossRefGoogle Scholar
Kröner, A and Stern, RJ (2004) Africa: Pan-African orogeny. Encyclopedia of Geology 1, 112.Google Scholar
Le Gall, B, Vétel, W and Morley, CK (2005) Inversion tectonics during continental rifting: the Turkana Cenozoic rifted zone, northern Kenya. Tectonics 24, doi: 10.1029/2004TC001637.CrossRefGoogle Scholar
Linol, B, de Wit, MJ, Barton, E, de Wit, MMJ and Guillocheau, F (2016) U–Pb detrital zircon dates and source provenance analysis of Phanerozoic sequences of the Congo Basin, central Gondwana. Gondwana Research 29, 208–19.CrossRefGoogle Scholar
Ludwig, KR (2012) User’s Manual for Isoplot 3.7–-4.15: A Geochronological Toolkit for Microsoft Excel. Berkeley, CA: Berkeley Geochronology Center Special Publication No. 5.Google Scholar
Maboko, MAH (1995) Neodymium isotopic constraints on the protolith ages of rocks involved in Pan-African tectonism in the Mozambique Belt of Tanzania. Journal of the Geological Society, London 152, 911–6.CrossRefGoogle Scholar
Maboko, MAH and Nakamura, E (1996) Nd and Sr isotopic mapping of the Archaean–Proterozoic boundary in southeastern Tanzania using granites as probes for crustal growth. Precambrian Research 77, 105–15.CrossRefGoogle Scholar
Maluski, H, Coulon, C, Popoff, MT and Baudin, P (1995) 40Ar/39Ar chronology, petrology and geodynamic setting of Mesozoic to early Cenozoic magmatism from the Benue Trough, Nigeria. Journal of the Geological Society, London 152, 311–26.CrossRefGoogle Scholar
McConnell, RB (1972) Geological development of the rift system of eastern Africa. Geological Society of America Bulletin 83, 2549–72.CrossRefGoogle Scholar
McDougall, IAN and Brown, FH (2009) Timing of volcanism and evolution of the northern Kenya Rift. Geological Magazine 146, 3447.CrossRefGoogle Scholar
McGuire, M, Serra, S and Day, R (1985) Surface Geological Evaluation, Block 10 Concession, NW Kenya. Internal Report. Houston, TX: Amoco Production Company.Google Scholar
Menzies, M, Gallagher, K, Yelland, A and Hurford, AJ (1997) Volcanic and non-volcanic rifted margins of the Red Sea and Gulf of Aden: crustal cooling and margin evolution in Yemen. Geochimica et Cosmochimica Acta 61, 2511–27.CrossRefGoogle Scholar
Miall, AD (1996) The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis, and Petroleum Geology. New York: Springer-Verlag, 582 pp.Google Scholar
Möller, A, Mezger, K and Schenk, V (1998) Crustal age domains and the evolution of the continental crust in the Mozambique Belt of Tanzania: combined Sm–Nd, Rb–Sr, and Pb–Pb isotopic evidence. Journal of Petrology 39, 749–83.CrossRefGoogle Scholar
Morag, N, Avigad, D, Gerdes, A, Belousova, E and Harlavan, Y (2011) Detrital zircon Hf isotopic composition indicates long-distance transport of north Gondwana Cambrian–Ordovician sandstones. Geology 39, 955–8.CrossRefGoogle Scholar
Morley, CK, Karanja, FM, Wescott, WA, Stone, DM, Harper, RM, Wigger, ST and Day, RA (1999) Geology and geophysics of the Western Turkana Basins, Kenya In Geoscience of Rift Systems—Evolution of East Africa (ed. Morley, CK), pp. 1954. American Association of Petroleum Geologists Studies in Geology 44.Google Scholar
Morley, CK, Wescott, WA, Stone, DM, Harper, RM, Wigger, ST and Karanja, FM (1992) Tectonic evolution of the northern Kenyan Rift. Journal of the Geological Society, London 149, 333–48.CrossRefGoogle Scholar
Mortimer, E, Kirstein, LA, Stuart, FM and Strecker, MR (2016) Spatio-temporal trends in normal-fault segmentation recorded by low-temperature thermochronology: Livingstone fault scarp, Malawi Rift, East African Rift System. Earth and Planetary Science Letters 455, 6272.CrossRefGoogle Scholar
Morton, A, Ellis, D, Fanning, M, Jolly, D and Whitham, A (2012) The importance of an integrated approach to provenance studies: a case study from the Paleocene of the Faroe-Shetland Basin, NE Atlantic. In Mineralogical and Geochemical Approaches to Provenance (eds Rasbury, ET, Hemming, SR and Riggs, NR), pp. 1–12. Geological Society of America Special Papers no. 487.CrossRefGoogle Scholar
Mosley, PN (1993) Geological evolution of the late Proterozoic “Mozambique Belt” of Kenya. Tectonophysics 221, 223–50.CrossRefGoogle Scholar
Murray-Hughes, R (1933) Notes on the Geological Succession, Tectonics and Economic Geology of the Western Half of the Kenya Colony. Nairobi: Report of the Geological Survey of Kenya No. 3, 8 pp.Google Scholar
Næraa, T, Scherstén, A, Rosing, MT, Kemp, AIS, Hoffmann, JE, Kokfelt, TF and Whitehouse, MJ (2012) Hafnium isotope evidence for a transition in the dynamics of continental growth 3.2 Gyr ago. Nature 485, 627.CrossRefGoogle ScholarPubMed
Neumaier, M, Tiercelin, JJ, Nalpas, T and Castillo, JM (2014) Basin analysis and petroleum systems modeling of the Lokichar Basin (Kenya). In AAPG International Conference and Exhibition: The Spirit Between Continents: Energy Geosciences in a Changing World. Istanbul, Turkey. 14–17 September 2014. Abstract. AAPG Search and Discovery Article #90194.Google Scholar
Nutz, A, Schuster, M, Boës, X and Rubino, JL (2017) Orbitally-driven evolution of Lake Turkana (Turkana Depression, Kenya, EARS) between 1.95 and 1.72 Ma: a sequence stratigraphy perspective. Journal of African Earth Sciences 125, 230–43.CrossRefGoogle Scholar
O’Connor, PM, Sertich, JJW and Manthi, FK (2011) A pterodactyloid pterosaur from the Upper Cretaceous Lapurr Sandstone, west Turkana, Kenya. Anais da Academia Brasileira de Ciências 83, 309–15.CrossRefGoogle ScholarPubMed
Oliveira, E, McNaughton, N, Windley, B, Carvalho, M and Nascimento, R (2015) Detrital zircon U–Pb geochronology and whole-rock Nd-isotope constraints on sediment provenance in the Neoproterozoic Sergipano Orogen: from early passive margins to late foreland basins. Tectonophysics 662, 183–94.CrossRefGoogle Scholar
Owusu, Agyemang PC, Roberts, EM and Jelsma, HA (2016) Late Jurassic–Cretaceous fluvial evolution of central Africa: insights from the Kasai-Congo Basin, Democratic Republic Congo. Cretaceous Research 67, 2543.CrossRefGoogle Scholar
Pearce, JA, Harris, NB and Tindle, AG (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology 25, 956–83.CrossRefGoogle Scholar
Permenter, JL and Oppenheimer, C (2007) Volcanoes of the Tibesti massif (Chad, northern Africa). Bulletin of Volcanology 69, 609–26.CrossRefGoogle Scholar
Pouclet, A, Bellon, H and Bram, K (2016) The Cenozoic volcanism in the Kivu Rift: assessment of the tectonic setting, geochemistry, and geochronology of the volcanic activity in the south-Kivu and Virunga regions. Journal of African Earth Sciences 121, 219–46.CrossRefGoogle Scholar
Purcell, P (2014) Oil and gas exploration in east Africa: a brief history. AAPG Search and Discovery Article #30388.Google Scholar
Purcell, PG (2017) Re-imagining and re-imaging the development of the East African Rift. Petroleum Geoscience 24, 2140.CrossRefGoogle Scholar
Reeves, CV, Karanja, FM and Macleod, IN (1987) Geophysical evidence for a failed Jurassic rift and triple junction in Kenya. Earth and Planetary Science Letters 81, 299311.CrossRefGoogle Scholar
Rino, S, Kon, Y, Sato, W, Maruyama, S, Santosh, M and Zhao, D (2008) The Grenvillian and Pan-African orogens: world’s largest orogenies through geologic time, and their implications on the origin of superplume. Gondwana Research 14, 5172.CrossRefGoogle Scholar
Roberts, EM, Stevens, NJ, O’Connor, PM, Dirks, PHGM, Gottfried, MD, Clyde, WC, Armstrong, RA, Kemp, AIS and Hemming, S (2012) Initiation of the western branch of the East African Rift coeval with the eastern branch. Nature Geoscience 5, 289–94.CrossRefGoogle Scholar
Rubatto, D (2002) Zircon trace element geochemistry: partitioning with garnet and the link between U–Pb ages and metamorphism. Chemical Geology 184, 123–38.CrossRefGoogle Scholar
Savage, RJ and Williamson, PG (1978) The early history of the Turkana Depression. In Geological Background to Fossil Man: Recent Research in the Gregory Rift Valley, East Africa (ed. Bishop, WW), pp. 375–94. Geological Society of London, Special Publication no. 6.CrossRefGoogle Scholar
Schaltegger, U, Fanning, CM, Günther, D, Maurin, JC, Schulmann, K and Gebauer, D (1999) Growth, annealing and recrystallization of zircon and preservation of monazite in high-grade metamorphism: conventional and in-situ U–Pb isotope, cathodoluminescence and microchemical evidence. Contributions to Mineralogy and Petrology 134, 186201.CrossRefGoogle Scholar
Sereno, PC, Beck, AL, Dutheil, DB, Gado, B, Larsson, HC, Lyon, GH, Marcot, JD, Rauhut, OW, Sadleir, RW, Sidor, CA and Varricchio, DD (1998) A long-snouted predatory dinosaur from Africa and the evolution of spinosaurids. Science 282, 1298–302.CrossRefGoogle ScholarPubMed
Sertich, J, Manthi, FK, Sampson, S, Loewen, M and Getty, M (2006) Rift valley dinosaurs: a new Late Cretaceous vertebrate fauna from Kenya. Journal of Vertebrate Paleontology 26, 124AGoogle Scholar
Sleep, NH (1996) Lateral flow of hot plume material ponded at sublithospheric depths. Journal of Geophysical Research: Solid Earth 101, 28065–83.CrossRefGoogle Scholar
Sláma, J and Košler, J (2012) Effects of sampling and mineral separation on accuracy of detrital zircon studies. Geochemistry, Geophysics, Geosystems 13, doi: 10.1029/2012GC004106.CrossRefGoogle Scholar
Söderlund, U, Patchett, PJ, Vervoort, JD and Isachsen, CE (2004) The 176 Lu decay constant determined by Lu–Hf and U–Pb isotope systematics of Precambrian mafic intrusions. Earth and Planetary Science Letters 219, 311–24.CrossRefGoogle Scholar
Stankiewicz, J and de Wit, MJ (2006) A proposed drainage evolution model for central Africa—did the Congo flow east? Journal of African Earth Sciences 44, 7584.CrossRefGoogle Scholar
Taylor, SR and McLennan, SM (1985) The Continental Crust: Its Composition and Evolution: An Examination of the Geochemical Record Preserved in Sedimentary Rocks. Oxford: Blackwell Scientific.Google Scholar
Tiercelin, JJ, Potdevin, JL, Morley, CK, Talbot, MR, Bellon, H, Rio, A, Le Gall, B and Vétel, W (2004) Hydrocarbon potential of the Meso-Cenozoic Turkana depression, northern Kenya. I. Reservoirs: depositional environments, diagenetic characteristics, and source rock-reservoir relationships. Marine and Petroleum Geology 21, 4162.CrossRefGoogle Scholar
Tiercelin, JJ, Potdevin, JL, Thuo, PK, Abdelfettah, Y, Schuster, M, Bourquin, S and Ruffet, G (2012a) Stratigraphy, sedimentology and diagenetic evolution of the Lapur Sandstone in northern Kenya: implications for oil exploration of the Meso-Cenozoic Turkana depression. Journal of African Earth Sciences 71, 4379.CrossRefGoogle Scholar
Tiercelin, JJ, Thuo, P, Potdevin, JL and Nalpas, T (2012b) Hydrocarbon prospectivity in Mesozoic and early–middle Cenozoic rift basins of central and northern Kenya, Eastern Africa. In Tectonics and Sedimentation: Implications for Petroleum Systems (ed. Gao, D), pp. 129. Tulsa, OK: American Association of Petroleum Geologists Memoir no. 100.Google Scholar
Tucker, RT, Roberts, EM, Hu, Y, Kemp, AI and Salisbury, SW (2013) Detrital zircon age constraints for the Winton Formation, Queensland: contextualizing Australia’s Late Cretaceous dinosaur faunas. Gondwana Research 24, 767–79.CrossRefGoogle Scholar
Van Achterbergh, E, Ryan, CG, Jackson, SE and Griffin, WL (2001) Appendix 3, data reduction software for LA-ICP-MS. In Laser-Ablation-ICPMS in the Earth Sciences: Principles and Applications (ed. Sylvester, P), pp. 239–43. Ottawa, ON: Mineralogical Association of Canada, Short Course Series.Google Scholar
Vincens, A, Tiercelin, JJ and Buchet, G (2006) New Oligocene–early Miocene microflora from the southwestern Turkana Basin: palaeoenvironmental implications in the northern Kenya Rift. Palaeogeography, Palaeoclimatology, Palaeoecology 239, 470–86.CrossRefGoogle Scholar
Walsh, J (1969) Geology of the Eldama Ravine-Kabarnet Area: Degree Sheet 34 SE Quarter (No. 83). Nairobi: Ministry of Natural Resources, Geological Survey of Kenya.Google Scholar
Walsh, J and Dodson, RG (1969) Geology of Northern Turkana. Nairobi: Geological Survey of Kenya Report no. 82.Google Scholar
Weishampel, DB, Barrett, PM, Coria, RA, Le Loeuff, J, Xing, X, Xijin, Z, Sahni, A, Gomani, EM and Noto, CR (2004) Dinosaur distribution. In The Dinosauria, 2nd ed. (eds Weishampel, DB, Dodson, P and Osmolska, H), pp. 571606. Berkeley: University of California Press.CrossRefGoogle Scholar
Wescott, WA, Morley, CK and Karanja, FM (1993) Geology of the “Turkana grits” in the Lariu Range and Mt. Porr areas, southern Lake Turkana, northwestern Kenya. Journal of African Earth Sciences (and the Middle East) 16, 425–35.CrossRefGoogle Scholar
Wescott, WA, Wigger, ST, Stone, DM and Morley, CK (1999) Geology and geophysics of the Lotikipi Plain. Geoscience of Rift Systems—Evolution of East Africa (ed. Morley, CK), pp. 55–65. American Association of Petroleum Geologists Studies in Geology 44.Google Scholar
Wiedenbeck, M, Hanchar, JM, Peck, WH, Sylvester, P, Valley, J, Whitehouse, M, Kronz, A, Morishita, Y, Nasdala, L, Fiebig, J and Franchi, I (2004) Further characterisation of the 91500 zircon crystal. Geostandards and Geoanalytical Research 28, 939.CrossRefGoogle Scholar
Williamson, PG and Savage, RJ (1986) Early rift sedimentation in the Turkana Basin, northern Kenya. In Sedimentation in the African Rifts (eds Frostick, LE, Renaut, RW, Reid, I and Tiercelin, JJ), pp. 267–83. Geological Society of London, Special Publication no. 25.Google Scholar
Wilson, M, Guiraud, R, Moreau, C and Bellion, YC (1998) Late Permian to Recent magmatic activity on the African–Arabian margin of Tethys In Petroleum Geology of North Africa (eds MacGregor, DS, Moody, RTJ and Clark-Lowes, DD), pp. 231–63. Geological Society of London, Special Publication no. 132.Google Scholar
Wolfenden, E, Ebinger, C, Yirgu, G, Deino, A and Ayalew, D (2004) Evolution of the northern Main Ethiopian Rift: birth of a triple junction. Earth and Planetary Science Letters 224, 213–28.CrossRefGoogle Scholar
Woodhead, JD and Hergt, JM (2005) A preliminary appraisal of seven natural zircon reference materials for in situ Hf isotope determination. Geostandards and Geoanalytical Research 29, 183–95.CrossRefGoogle Scholar
Yang, J, Cawood, PA, Du, Y, Huang, H, Huang, H and Tao, P (2012) Large Igneous Province and magmatic arc sourced Permian–Triassic volcanogenic sediments in China. Sedimentary Geology 261, 120–31.CrossRefGoogle Scholar
Yao, J, Shu, L and Santosh, M (2011) Detrital zircon U–Pb geochronology, Hf-isotopes and geochemistry – new clues for the Precambrian crustal evolution of Cathaysia Block, south China. Gondwana Research 20, 553–67.CrossRefGoogle Scholar
Zanettin, B, Visentin, EJ, Bellieni, G, Piccirillo, EM and Rita, F (1983) Le volcanisme du Bassin du Nord-Turkana (Kenya): age, succession et évolution structurale. In Rifts et Fossés Anciens. Bulletin des Centres de Recherches Exploration–Production Elf-Aquitaine, Vol. 7 (eds Popoff, M and Tiercelin, JJ), pp. 249–55. Marseille: Faculté des sciences et techniques de Saint-Jérôme.Google Scholar
Zheng, Y-F, Zhang, S-B, Zhao, Z-F, Wu, Y-B, Li, X, Li, Z and Wu, F-Y (2007) Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: implications for growth and reworking of continental crust. Lithos 96, 127–50.CrossRefGoogle Scholar
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Sedimentary provenance and maximum depositional age analysis of the Cretaceous? Lapur and Muruanachok sandstones (Turkana Grits), Turkana Basin, Kenya
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Sedimentary provenance and maximum depositional age analysis of the Cretaceous? Lapur and Muruanachok sandstones (Turkana Grits), Turkana Basin, Kenya
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