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Evidence for Mesoproterozoic Components in the Arabian-Nubian Shield

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The Geology of the Arabian-Nubian Shield

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Abstract

This chapter reviews and summarizes the early ideas on the existence of Mesoproterozoic components in the Arabian-Nubian Shield (ANS). It sheds more light on their significance in crustal evolution of the ANS. Nowadays, there is a general agreement among geologists that the Late Mesoproterozoic to Cambrian period bears the most remarkable geological record in Earth’s history. It began with the assembly of Rodinia supercontinent (1300–900 Ma) and ended by the amalgamation of Gondwana supercontinent (around 550 Ma). It is widely accepted that the ANS were formed by juvenile magmatic arc accretion and subsequent shield-wide post-tectonic magmatism. However, the recorded Mesoproterozoic crust, with subordinate Palaeoproterozoic and rare Archaean components, proves that ANS is less juvenile than previously thought, and may provide important clues for the reconstruction of the crustal evolution of the ANS. Recent studies by several workers have shown that inherited zircon grains from igneous rocks within the ANS may provide evidence for Mesoproterozoic crustal growth. The Mesoproterozoic components of the ANS were interpreted as pervasively reworked pre-existing crust during the Pan-African orogeny, which was responsible for the final juxtaposition of the collage of terranes now seen, e.g. reworked pre-Neoproterozoic crustal fragments at Sa’al Mesoproterozoic rocks, Wadi Rutig volcano-sedimentary succession and Wadi Solaf metapsammitic and granodioritic biotite gneisses in Sinai (Egypt); Khida subterrane in eastern Saudi Arabia; the arc–gneiss collages of the Precambrian basement of Yemen and the eastern Ethiopian–northwestern Somalian crustal block. Sediments are good natural samplers of the existing continental crust at the time of erosion and sedimentation. Several workers have presented detrital zircon isotopic dataset from the Palaeozoic sedimentary sequences of the ANS (e.g. Meinhold et al. 2020). They interpreted the Ediacaran to middle Tonian zircon grains as being derived from igneous rocks of the ANS, whereas Palaeoproterozoic and Archaean grains were interpreted as a primary derivation from Palaeoproterozoic and Archaean basement found in some parts of the ANS or crustal components of the eastern Saharan Metacraton. This is consistent with palaeocurrent indicators, which suggest sediment transport from the hinterland of Gondwana. In the light of the above, future efforts to understand ANS crustal evolution will require more zircon geochronology and related studies to answer two main questions: (1) how isotopically juvenile Neoproterozoic magmas were contaminated with pre-Neoproterozoic zircon? and (2) was zircon assimilated from unexposed older crust that underlies the contaminated shield or derived from Neoproterozoic sediments sourced from a neighbouring pre-Neoproterozoic craton?

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References

  • Abd El-Naby HH, Frisch W, Siebel W (2008) Tectonic–metamorphic evolution of the Wadi Hafafit culmination (central Eastern Desert, Egypt). Implication for Neoproterozoic core complex exhumation in NE Africa. Geol Acta 6:293–312

    Google Scholar 

  • Abdel-Monem AA, Hurley PM (1979) U-Pb dating of zircon from psammitic gneisses, Wadi Abu Rosheid-Wadi Sikait area, Egypt. Institute of Applied Geology Bulletin, King Abdulaziz University Jeddah, Saudi. Arabia 2:165–170

    Google Scholar 

  • Abdel-Rahman AM (1995) Tectonic-magmatic stages of shield evolution: the Pan-African belt in northeastern Egypt. Tectonophysics 242:223–240

    Article  Google Scholar 

  • Abdelrahman EM, Matheis G, Schandelmeier H, Karfis MA, Gadir I, El Khedir M (1993) Evolution of the Keraf back-arc basin: constraints on the Nubian Shield margin. In: Thorweihe U, Schandelmeier H (eds) Geoscientific research in NE Africa. Balkema, Amsterdam, pp 93–98

    Google Scholar 

  • Abdelsalam MG, Stern RJ, Copeland P, Elfaki EM, Elhur B, Ibrahim FM (1998) The Neoproterozoic Keraf Suture in NE Sudan: sinistral transpression along the eastern margin of West Gondwana. J Geol 106:133–147

    Article  Google Scholar 

  • Abdelsalam MG, Liegeois JP, Stern RJ (2002) The Saharan Metacraton. J Afr Earth Sci 34:119–136

    Article  Google Scholar 

  • Abdelsalam M, Gao S, Liégeois J-P (2011) Upper mantle structure of the Saharan Metacraton. J Afr Earth Sci 60(5):328–336

    Article  Google Scholar 

  • Abu Anbar M, Solís Pichardo G, Hernández Bernal MS, Morales, Contreras J, Hernández Treviño T (2004) Sm-Nd and Rb-Sr isotopes of Feiran gneisses and amphibolites: evidences of Pre-Pan-African continental crust in Sinai, Egypt. In: 6th International Conference Geochemical, Alex Univ, Egypt, 727–745

    Google Scholar 

  • Abu El-Enen MM, Whitehouse MJ (2013) The Feiran-Solaf metamorphic complex, Sinai, Egypt: geochronological and geochemical constraints on its evolution. Precambr Res 239:106–125

    Article  Google Scholar 

  • Agar RA, Stacey JS, Whitehouse MJ (1992) Evolution of the southern Afif terrane—a geochronologic study. Saudi Arabian Deputy Ministry for Mineral Resource Open File Report DGMR-OF-10–15, 41p

    Google Scholar 

  • Akaad MK, Noweir AM (1980) Geology and lithostratigraphy of the Arabian Desert Orogenic Belt of Egypt between Lat. 25 35′and 26 30′. Bull Inst Appl Geol King Abdulaziz Univ 3:127–135

    Google Scholar 

  • Ali KA, Stern RJ, Manton WI, Johnson PR, Mukherjee SK (2010) Neoproterozoic diamictite in the Eastern Desert of Egypt and Northern Saudi Arabia: evidence of ~750 Ma glaciation in the Arabian Nubian Shield? Int J Earth Sci 99:705–726

    Article  Google Scholar 

  • Ali K, Andresen A, Manton WI, Stern RJ, Somar A, Maurice AE (2012) U-Pb zircon dating and Sr-Nd-Hf isotopic evidence to support a juvenile origin of the ~634 Ma El Shalul granitic gneiss dome, Arabian-Nubian Shield. Geol Mag 149:783–797

    Article  Google Scholar 

  • Andresen A, El-Rus MA, Myhre PI, Boghdady GY, Corfu F (2009) U-Pb TIMS age constraints on the evolution of the Neoproterozoic Meatiq Gneiss Dome. Int J Earth Sci, Eastern Desert, Egypt. https://doi.org/10.1007/s00531-007-0276-x

    Book  Google Scholar 

  • Augland LE, Andresen A, Boghdady GY (2012) U-Pb ID-TIMS dating of igneous and metaigneous rocks from the El-Sibai area: time constraints on the tectonic evolution of the Central Eastern Desert, Egypt. Int J Earth Sci 101:25–37

    Article  Google Scholar 

  • Avigad D, Sandler A, Kolodner K, Stern R, McWilliams M, Miller N, Beyth M (2005) Mass-production of Cambro-Ordovician quartz-rich sandstone as a consequence of chemical weathering of Pan-African terranes: environmental implications. Earth Planet Sci Lett 240:818–826

    Article  Google Scholar 

  • Avigad D, Gerdes A, Morag N, Bechstädt T (2012) Coupled U-Pb-Hf of detrital zircons of Cambrian sandstones from Morocco and Sardinia: Implications for provenance and Precambrian crustal evolution of North Africa. Gondwana Res 21(2–3):690–703

    Article  Google Scholar 

  • Baubron JC, Delfour J, Vialette J (1976) Geochronological measurements (Rb-Sr; K-Ar) on rocks of the Arabian Shield. French Bureau de Recherches Géologiques et Minières. Technical Record 76-JED-22, 152p

    Google Scholar 

  • Be’eri-Shlevin Y, Katzir Y, Whitehouse MJ, Kleinhanns IC (2009a) Contribution of pre Pan-African crust to formation of the Arabian-Nubian Shield: new secondary ionization mass spectrometry U-Pb and O studies of zircon. Geology 37:899–902

    Article  Google Scholar 

  • Be’eri-Shlevin Y, Katzir Y, Whitehouse MJ (2009b) Post-collisional tectonomagmatic evolution in the northern Arabian-Nubian Shield: time constraints from ion-probe U-Pb dating of zircon. J Geol Soc Lond 166:71–85

    Article  Google Scholar 

  • Be’eri-Shlevin Y, Eyal M, Eyal Y, Whitehouse MJ, Litvinovsky B (2012) The Sa’al volcano-sedimentary complex (Sinai, Egypt), a latest Mesoproterozoic volcanic arc in the northern Arabian Nubian Shield. Geology 40:403–406

    Article  Google Scholar 

  • Bea F, Montero P, Abu Anbar M, Talavera C (2011a) SHRIMP dating and Nd isotope geology of the Archean terranes of the Uweinat-Kamil inlier, Egypt-Sudan-Libya. Precambr Res 189:328–346

    Article  Google Scholar 

  • Bea F, Montero P, Abu Anbar M, Molina JF, Scarrow JH (2011b) The Bir Safsaf Precambrian inlier of South West Egypt revisited. A model for ~1.5 Ga TDM late Pan-African granite generation by crustal reworking. Lithos 125:897–914

    Article  Google Scholar 

  • Begg GC, Griffin WL, Natapov LM, O’Reilly SY, Grand SP, O’Neill CJ, Hronsky JMA, Poudjom Djomani Y, Swain CJ, Deen T, Bowden P (2009) The lithospheric architecture of Africa: Seismic tomography, mantle petrology, and tectonic evolution. Geosphere 5:23–50

    Article  Google Scholar 

  • Berhe SM (1990) Ophiolites in Northeast and East Africa: implications for Proterozoic crustal growth. J Geol Soc Lond 147:41–57

    Article  Google Scholar 

  • Bielski M (1982) Stages in the Arabian-Nubian Massif in Sinai. Unpublished PhD thesis, Hebrew Univ., Jerusalem, 155p

    Google Scholar 

  • Bingen B, Jacobs J, Viola G, Henderson IHC, Skara Ø, Boyd R, Thomas RJ, Solli A, Key RM, Daudi EXF (2009) Geochronology of the Precambrian crust in the Mozambiquebelt in NE Mozambique and implications for Gondwana assembly. Precambr Res 170:231–255

    Article  Google Scholar 

  • Bregar M, Bauernhofer A, Pelz K, Kloetzli U, Fritz H, Neumayr P (2002) A late Neoproterozoic magmatic core complex in the Eastern Desert of Egypt: emplacement of granitoids in a wrench-tectonic setting. Precambr Res 118:59–82

    Article  Google Scholar 

  • Burke K, MacGregor DS, Cameron NR (2003) Africa’s petroleum systems: four tectonic “Aces” in the past 600 million years. In: Arthur TJ, MacGregor DS, Cameron NR (eds) Geological Society. Special Publications, London, pp 21–60

    Google Scholar 

  • Cahen L, Snelling NJ, Delhal J, Vail JR (1984) The geochronology and evolution of Africa. Clarendon Press, Oxford, p 512

    Google Scholar 

  • Calvez JY, Kemp J (1982) Geochronological investigations in the Mahd adh Dhahab quadrangle, central Arabian Shield, Saudi Arabian Deputy Ministry for Mineral Resources Technical Record BRGM-TR-02-5, 41p

    Google Scholar 

  • Calvez JV, Delfour J, Feybesse JL (1985) 2000-million-year old inherited zircons in plutonic rocks from the Al Amar region: New evidence for an Early Proterozoic basement in the eastern Arabian Shield? Saudi Arabian Deputy Ministry for Mineral Resources Open File Report BRGM-OF-05-11, 28 p

    Google Scholar 

  • Castaing C, Feybesse JL, Thieblemont D, Triboulet C, Chevremont P (1994) Paleogeographical reconstructions of the Pan-African/Brasiliano orogen:closure of an oceanic domain or intracontinental convergence between major blocks? Precambr Res 69:327–344

    Article  Google Scholar 

  • Cawood PA (2005) Terra Australis Orogen: rodinia breakup and development of the Pacific and Iapetus margins of Gondwana during the Neoproterozoic and Paleozoic. Earth-Sci Rev 69:249–279

    Article  Google Scholar 

  • Claesson S, Pallister JS, Tatsumoto M (1984) Samarium-neodymium data on two late Proterozoic ophiolites of Saudi Arabia and implications for crustal and mantle evolution. Contrib Mineral Petrol 85:244–252

    Article  Google Scholar 

  • Clifford TN (1970) The structural framework of Africa. In: Clifford TN, Gass IG (eds) African magmatism and tectonics. Edinburgh, Oliver and Boyd, pp 1–26

    Google Scholar 

  • Collins AS (2006) Madagascar and the amalgamation of Central Gondwana. Gondwana Res 9:3–16

    Article  Google Scholar 

  • Collins AS, Windley BF (2002) The tectonic evolution of central and northern Madagascar and its place in the final assembly of Gondwana. J Geol 110:325–339

    Article  Google Scholar 

  • Collins AS, Pisarevsky SA (2005) Amalgamating eastern Gondwana; the evolution of the Circum-Indian Orogens. Earth Sci Rev 71:229–270

    Article  Google Scholar 

  • Collins GS, Melosh HJ, Osinski GS (2012) The impact-cratering process. Elements 8:25–30

    Article  Google Scholar 

  • Condie KC (2001) Continental growth during formation of Rodinia at l.35—0.9Ga. Gondwana Res 4:5–16

    Article  Google Scholar 

  • D’Amico C, Ibrahim HA, Sassi NP (1981) Outline of the Somali Basement. Geol Rundsch 70–3:882–896

    Article  Google Scholar 

  • De Waele B (2005) The Proterozoic geological history of the Irumide belt, Zambia. PhD Thesis, Curtin University of Technology, Perth, 468 p

    Google Scholar 

  • De Waele B, Kampunzu AB, Mapani BSE, Tembo F (2006) The Mesoproterozoic Irumide belt of Zambia. J Afr Earth Sci 46:36–70

    Article  Google Scholar 

  • De Waele B, Johnson SP, Pisarevsky SA (2008) Palaeoproterozoic to Neoproterozoic growth and evolution of the eastern Congo Craton: its role in the Rodinia puzzle. Precambr Res 160:127–141

    Article  Google Scholar 

  • Delfour J (1980) Geologic, tectonic and metallogenic evolution of the northern part of the Precambrian Arabian shield (Kingdom of Saudi Arabia). Bulletin Bureau des Récherches Géologiques et Minieres 11:1–20

    Google Scholar 

  • Dixon TH, Golombek MP (1988) Late Precambrian crustal accretion rates in Northeast Africa and Arabia. Geology 16(11):991–994

    Article  Google Scholar 

  • El Gaby S (1983) Architecture of the Egyptian basement complex. Inter Basement Tectonics Assoc Publ 5:1–18

    Google Scholar 

  • El Gaby S, Khudeir AA, Youssef M, Kamal El Din G (1988a) Low pressure metamorphism in Hammamat sediments at Wadi Um Had area, central Eastern Desert, Egypt. Bull Fac Sci Assuit Univ 17:51–71

    Google Scholar 

  • El Gaby S, List F, Tehrani R (1988b) Geology, evolution and metallogenesis of the Pan-African belt in Egypt. In: El-Gaby S, Greiling RO (eds) The Pan-African Belt of Northeast Africa and Adjacent Areas. Vieweg and Sohn, Weisbaden, pp 17–68

    Google Scholar 

  • El Gaby S, List F, Tehrani R (1990) The basement complex of the Eastern Desert and Sinai. In: Said R (ed) The geology of Egypt. Balkema, Rotterdam, pp 175–200

    Google Scholar 

  • El-Manharawy MA (1977) Geochronological investigations of some basement rocks in the central Eastern Desert, Egypt, between lat. 25° and 26°N. Unpublished PhD thesis, Cairo Univ., 211 p

    Google Scholar 

  • El-Shafei MK, Kusky TM (2003) Structural and tectonic evolution of the Neoproterozoic Feiran-Solaf metamorphic belt Sinai Peninsula: implications for the closure of the Mozambique ocean. Precambr Res 123:269–293

    Article  Google Scholar 

  • Fleck RJ, Coleman RG, Cornwall HR, Greenwood WR, Hadley DG, Prinz WC, Ratte JS, Schmidt DL (1973) Potassium-argon Geochronology of the Arabian Shield. United States Department of International Geological Survey, Saudi Arabia Project Report 165, 1–40

    Google Scholar 

  • Fowler A, Khamees H, Dowidar H (2007) El-Sibai gneissic complex, Central Eastern Desert, Egypt: folded nappes and syn-kinematic gneissic granitoid sheets—not a core complex. J Afr Earth Sci 49:119–135

    Article  Google Scholar 

  • Fritz H, Tenczer V, Wallbrecher CA, Hauzenberger E, Hoinkes G, Muhongo S, Mogessie A (2005) Central Tanzanian tectonic map: a step forward to decipher Proterozoic structural events in the East AfricanOrogen. Tectonics 24, TC6013. http://dx.doi.org/10.1029/2005TC001796

  • Fritz H, Abdelsalam M, Ali KA, Bingen B, Collins AS, Fowler AR, Ghebreab W, Hauzenberger CA, Johnson PR, Kusky TM, Macey P, Muhongo S, Stern RJ, Viola G (2013) Orogen styles in the East African Orogen: a review of the Neoproterozoic to Cambrian tectonic evolution. J Afr Earth Sci 86:65–106

    Article  Google Scholar 

  • Garfunkel Z (2002) Early Paleozoic sediments of NE Africa and Arabia: products of continental-scale erosion, sediment transport and deposition. Isr J Earth Sci 51:135–156

    Article  Google Scholar 

  • Garson S, Shalaby IM (1976) Precambrian-lower Palaeozoic plate tectonics and metallogenesis in the Red Sea region. Geol Assoc Can Spec Pap 14:574–596

    Google Scholar 

  • Garzanti E, Vermeesch P, Andò S, Vezzoli G, Valagussa M, Allen K, Kadi KA, Al-Juboury AIA (2013) Provenance and recycling of Arabian desert sand. Earth Sci Rev 120:1–19

    Article  Google Scholar 

  • Gellatly D (1960) Geology of the Las Dureh area, Burao district: Somalia Geological Survey Report no. 6, 40 p

    Google Scholar 

  • Gladkochub DP, Donskaya TV, Mazukabzov AM, Pisarevsky SA, Ernst RE, Stanevich AM (2016) The Mesoproterozoic mantle plume beneath the northern part of the Siberian craton. Russ Geol Geophys 57:672–686

    Article  Google Scholar 

  • Goodwin AM (1996) Principles of Precambrian geology. Academic Press, San Diego

    Google Scholar 

  • Grantham GH, Manhica ADST, Armstrong RA, Kruger FJ, Loubser M (2011) New SHRIMP, Rb/Sr and Sm/Nd isotope and whole rock chemical data from central Mozambique and western Dronning Maud Land, Antarctica: implications for the nature of the eastern margin of the Kalahari Craton and the amalgamation of Gondwana. J Afr Earth Sci 59:74–100

    Article  Google Scholar 

  • Grotzinger JP, Knoll AH (1996) Stromatolites in Precambrian carbonates: evolutionary mileposts or environmental dipsticks? Annu Rev Earth Planet Sci 27:313–358

    Article  Google Scholar 

  • Habib ME, Ahmed AA, El Nady OM (1985a) Two orogenies in the Meatiq area of the Central Eastern Desert, Egypt. Precambr Res 30:83–111

    Article  Google Scholar 

  • Habib ME, Ahmed AA, El Nady OM (1985b) Tectonic evolution of the Meatiq infrastructure, Central Eastern Desert, Egypt. Tectonics 4:613–627

    Article  Google Scholar 

  • Hamimi Z, El Amawy MA, Wetait M (1994) Geology and structural evolution of El Shalul dome and environs, Central Eastern Desert, Egypt. Egypt J Geol 38:575–595

    Google Scholar 

  • Hargrove US, Stern RJ, Kimura J-I, Manton WI, Johnson PR (2006) How juvenile is the Arabian-Nubian Shield? Evidence from Nd isotopes and pre-Neoproterozoic inherited zircon in the Bi’r Umq suture zone, Saudi Arabia. Earth Planet Sci Lett 252:308–326

    Article  Google Scholar 

  • Harms U, Schandelmeier H, Darbyshire DPF (1990) Pan-African reworked early/middle Proterozoic crust in NE Africa west of the Nile: Sr and Nd isotope evidence. J Geol Soc Lond 147:859–872

    Article  Google Scholar 

  • Harris NBW, Hawkesworth CJ, Ries AC (1984) Crustal evolution in northeast and East Africa from model Nd ages. Nature 309:773–776

    Article  Google Scholar 

  • Hartnady CJH, Joubert P, Stowe CW (1985) Proterozoic crustal evolution in southwestern Africa. Episodes 8:236–244

    Article  Google Scholar 

  • Hassan MA, Hashad AH (1990) Precambrian of Egypt. In: Said R (ed) The geology of Egypt. Balkema, Rotterdam, pp 201–245

    Google Scholar 

  • Hauzenberger CA, Bauernhofer AH, Hoinkes G, Wallbrecher E, Mathu EM (2004) Pan-African high pressure granulites from SE-Kenya: petrological and geothermobarometric evidence for a polycyclic evolution in the Mozambique belt. J Afr Earth Sci 40:245–268

    Article  Google Scholar 

  • Hauzenberger CA, Sommer S, Fritz H, Bauernhofer A, Kröner A, Hoinkes G, Wallbrecher E, Thöni M (2007) SHRIMP U-Pb zircon and Sm–Nd garnet ages from granulite facies basement of SE-Kenya: evidence for Neoproterozoicpolycyclic assembly of the Mozambique belt. J Geol Soc Lond 164:189–201

    Article  Google Scholar 

  • Hume WF (1934) Geology of Egypt 2, Part 1: The metamorphic rocks. Geol Surv Egypt, 293p

    Google Scholar 

  • Hunt JA (1958) Geology of the Adadleh area, Hargeisa and Berbera districts: Somaliland British Protectorate Geological Survey Report no. 2, 16 p

    Google Scholar 

  • Hunting Geology and Geophysics Ltd. (1974) Geology of the Jabal Al Uwaynat area, Libyan Arab Republic. Report to Industrial Research Centre, Department of Geological Research and Mining, Tripoli. Boreham Wood, U.K

    Google Scholar 

  • Huth A, Franz G, Schandelmeier H (1984) Magmatic and metamorphic rocks of NW Sudan: a reconnaissance survey. Berliner geowissenschaft liche Abhandlungen Reihe A50:7–21

    Google Scholar 

  • Jacobs J, Thomas RJ (2004) Himalayan-type indenter-escape tectonics model for the southern part of the late Neoproterozoic-early Paleozoic East-African-Antarctic Orogen. Geology 32:721–724

    Article  Google Scholar 

  • Jacobs J, Fanning CM, Henjes-Kunst F, Olesch M, Paech H-J (1998) Continuation of the Mozambique into East Antarctica: Grenville-age metamorphism and polyphase Pan-African high grade events in central Dronning Maud Land. J Geol 106:385–406

    Article  Google Scholar 

  • Johnson PR, Woldehaimanot B (2003) Development of the Arabian–Nubian shield: perspectives on accretion and deformation in the northern East African Orogen and the assembly of Gondwana. In: Yoshida M, Windley BF, Dasgupta S (eds) Proterozoic East Gondwana: supercontinent assembly and breakup, vol 206. Geol. Soc. Lond. Spec. Publ.:290–325

    Google Scholar 

  • Johnson PR, Andresen A, Collins AS, Fowler AR, Fritz H, Ghebreab W, Kusky T, Stern RJ (2011) Late Cryogenian-Ediacaran history of the Arabian-Nubian Shield: a review of depositional, plutonic, structural, and tectonic events in the closing stages of the northern East African Orogen. J Afr Earth Sci 61:167–232

    Article  Google Scholar 

  • Jöns N, Schenk V (2008) Relics of the Mozambique Ocean in the central East African Orogen: evidence from the Vohibory Block of southern Madagascar. J Metamorph Geol 26:17–28

    Google Scholar 

  • Jöns N, Schenk V (2011) The ultrahigh temperature granulites of southern Madagascar in a polymetamorphic context: implications for the amalgamation of the Gondwana supercontinent. Eur J Mineral 23:127–156

    Article  Google Scholar 

  • Kamal El Din GM, Khudeir AA, Greiling RO (1992) Tectonic evolution of a Pan-African gneiss culmination, Gabal El-Sibai area, Central Eastern Desert, Egypt. Zbl Geol Paläont Teil 1(1991):2637–2640

    Google Scholar 

  • Kazmin V (1971) The Precambrian of Ethiopia. Nature Phys Sci Lond 280:176–177

    Article  Google Scholar 

  • Kazmin V (1975) The Precambrian of Ethiopia and some aspects of the geology of the Mozambique Belt. Bull Geophys Obs Addis Ababa 15:27–43

    Google Scholar 

  • Kazmin V, Shifferaw A, Balch T (1978) The Ethiopian Basement: Stratigraphy and Possible Manner of Evolution. Geol Rundsch 67:531–546

    Article  Google Scholar 

  • Kemp J, Pellaton C, Calvez J V (1980) Geochronological investigatiom and geological history in the Precambrian of northwestern Saudi Arabia. Bureau des Recherches Gtologiques et Minieres Open File-01-1

    Google Scholar 

  • Kennedy WO (1964) The structural differentiation of Africa in the Pan-African tectonic episode. In: 8th Ann. Rep., Res. Inst. Afr. Geol., Leeds Univ., 48–49

    Google Scholar 

  • Kennedy WQ (1965) The influence of basement structure on the evolution of the coastal (Mesozoic and Tertiary) basins of Africa. Salt Basins around Africa. Institute of Petroleum, London, pp 7–16

    Google Scholar 

  • Kennedy A, Johnson PR, Kattan FH (2004) SHRIMP geochronology in the northern Arabian Shield, Part 1: Data acquisition, Saudi Geological Survey Open File Report SGS-OF-2004-11, 28 p

    Google Scholar 

  • Khudeir AA, El-Gaby S, Greiling RO, Kamal El Din GM (1992) Geochemistry and tectonic significance of polymetamorphosed amphibolites in the Gabal Sibai window, Central Eastern Desert, Egypt. In: 1st International conference on geology of the Arab World, Cairo Univ, 461–476

    Google Scholar 

  • Klerkx J (1980) Age and metamorphic evolution of the basement complex around Jabal al’Awaynat. In: Salim MJ, Busrewil MT (eds) The Geology of Libya 2. Academic Press, London, pp 901–906

    Google Scholar 

  • Klerkx J, Deutsch S (1977) Resultats preliminaires obtenus par la methode Rb/Sr sur l’age des formations Precambriennes de la region d’Uweinat (Libye). Musee R. l’Afr. Centrale. Déepart. Géeol. Minéeral Rapp Ann, 83–94

    Google Scholar 

  • Knoll AH, Semikhatov MA (1998) The genesis and time distribution of two distinctive Proterozoic stromatolitic microstructures. Palaios 13:407–421

    Article  Google Scholar 

  • Kröner A (1979) Pan-African mobile belts as evidence for a transitional tectonic regime from intraplate orogeny to plate margin orogeny. In: Al Shanti AMS (ed.) Evolution of the Arabian-Nubian Shield vol. 1, Institute of Applied Geology Bulletin 3:21–37

    Google Scholar 

  • Kröner A (1984) Late Precambrian plate tectonics and orogeny: a need to redefine the term Pan-African. In: Klerkx J, Michot J (eds) African Geology. Tervuren, Belgium, pp 23–28

    Google Scholar 

  • Kröner A (1985) Ophiolites and the evolution of tectonic boundaries in the late Proterozoic Arabian-Nubian shield of northeastern Africa and Arabia. Precambr Res 27:277–300

    Article  Google Scholar 

  • Kröner A, Sassi FP (1996) Evolution of the northern Somali basement: new constraints from zircon ages. J Afr Earth Sci 22:l–15

    Google Scholar 

  • Kröner A, Stern RJ (2004) Pan-African orogeny. In: Selley RC, Cocks LRM, Plimer IR (eds) Encyclopedia of Geology, 1. Elsevier, Amsterdam, pp 1–12

    Google Scholar 

  • Kröner A, Greiling R, Reischmann T, Hussein IM, Stern RJ, Durr S, Krüger J, Zimmer M (1987) Pan-African crustal evolution in the Nubian segment of Northeast Africa. Am Geophys Union Geodyn Ser 17:235–257

    Google Scholar 

  • Kröner A, Kruger J, Rashwan AA (1994) Age and tectonic setting of granitoid gneisses in the Eastern Desert of Egypt and south-west Sinai. Geol Rundsch 83:502–513

    Article  Google Scholar 

  • Küster D, Liégeois J-P (2001) Sr, Nd isotopes and geochemistry of the Bayuda Desert high-grade metamorphic basement (Sudan): An early Pan-African oceanic convergent margin, not the edge of the East Saharan ghost craton? Precambr Res 109(1):1–23

    Article  Google Scholar 

  • Küster D, Liégeois J-P, Matukov D, Sergeev S, Lucassen F (2008) Zircon geochronology and Sr, Nd, Pb isotope geochemistry of granitoids from Bayuda Desert and Sabaloka (Sudan): Evidence for a Bayudian event (920–900 Ma) preceding the Pan-African orogenic cycle (860–590 Ma) at the eastern boundary of the Saharan Metacraton. Precambr Res 164(1–2):16–39

    Article  Google Scholar 

  • Kusky TM, Abdelsalam M, Stern RJ, Tucker RD (2003) Evolution of the East African and related Orogens, and the assembly of Gondwana. Precambr Res 123:82–85

    Article  Google Scholar 

  • Lancelot JR, Bosch D (1991) A Pan African age for the HP–HT granulite gneisses of Zabargad Island; implications for the early stages of the Red Sea rifting. Earth Planet Sci Lett 107:539–549

    Article  Google Scholar 

  • Lewin A, Meinhold G, Hinderer M, Dawit EL, Bussert R (2018) Provenance of sandstones in Ethiopia during Late Ordovician and Carboniferous-Permian Gondwana glaciations: Petrography and geochemistry of the Enticho Sandstone and the Edaga Arbi Glacials. Sediment Geol 375:188–202

    Article  Google Scholar 

  • Li X-H, Abd El-Rahman Y, Abu Anbar M, Li J, Ling X-X, Wu L-G, Masoud AE (2018) Old continental crust underlying juvenile oceanic arc: Evidence from northern Arabian-Nubian Shield, Egypt. Geophys Res Lett 45:3001–3008

    Article  Google Scholar 

  • Li ZX, Bogdanova SV, Collins AS, Davidson A, DeWaele B, Ernst RE, Fitzsimons ICW, Fuck RA, Gladkochub DP, Jacobs J, Karlstrom KE, Lu S, Natapov LM, Pease V, Pisarevsky SA, Thrane K, Vernikovsky V (2008) Assembly, configuration, and break-up history of Rodinia: a synthesis. Precambr Res 160:179–210

    Article  Google Scholar 

  • Liégeois JP, Stern RJ (2010) Sr–Nd isotopes and geochemistry of granite–gneiss complexes from the Meatiq and Hafafit domes, Eastern Desert, Egypt: no evidence for pre-Neoproterozoic crust. J Afr Earth Sci 57:31–40

    Article  Google Scholar 

  • Lundmark AM, Andresen A, Hassan MA, Augland LE, Abu El-Rus MA, Boghdady GY (2012) Repeated magmatic pulses in the East African Orogen of Central Eastern Desert, Egypt: an old idea supported by new evidence. Gondwana Res 22:227–237

    Article  Google Scholar 

  • Manya S, Maboko MAH (2003) Dating basaltic volcanism in the Neoarchaean Sukumaland Greenstone Belt of the Tanzania Craton using the Sm–Nd method: implications for the geological evolution of the Tanzania Craton. Precambr Res 121:35–45

    Article  Google Scholar 

  • Meert JG (2003) A synopsis of events related to the assembly of eastern Gondwana. Tectonophysics 362:1–40

    Article  Google Scholar 

  • Meinhold G, Morton AC, Avigad D (2013) New insights into peri-Gondwana paleogeography and the Gondwana super-fan system from detrital zircon U-Pb ages. Gondwana Res 23:661–665

    Article  Google Scholar 

  • Meinhold G, Bassis A, Hinderer M, Lewin A, Berndt J (2020) Detrital zircon provenance of north Gondwana Palaeozoic sandstones from Saudi Arabia. Geological Magazine Pub, 24 June 2020. https://doi.org/10.1017/s0016756820000576

  • Möller A, Mezger K, Schenk V (2000) U-Pb dating of metamorphic minerals: Pan-African metamorphism and prolonged slow cooling of high pressure granulites in Tanzania East Africa. Precambr Res 104:123–146

    Article  Google Scholar 

  • Neumayr P, Mogessie P, Hoinkes G, Puhl J (1996) Geological setting of the Meatiq metamorphic core complex in the Eastern Desert of Egypt based on amphibolite geochemistry. J Afr Earth Sci 23(3):331–345

    Article  Google Scholar 

  • Pohl WL (1979) Metallogenic/Minerogenic Analysis—Contribution to the Differentiation between Mozambiquian Basement and Pan-African Superstructure in the Red Sea Region. Annals Geol Survey Egypt 9:32–44

    Google Scholar 

  • Reymer A, Schubert G (1986) Rapid growth of some major segments of continental crust. Geology 14(4):299–302

    Article  Google Scholar 

  • Ries AC, Shackleton RM, Graham RH, Fitches WR (1983) Pan-African structures, ophiolites and mélanges in the east Desert of Egypt: a traverse at 26 north. J Geol Soc Lond 140:75–95

    Article  Google Scholar 

  • Rino S, Kon Y, Sato W, Maruyama S, Santosh M, 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 Res 14:51–72

    Article  Google Scholar 

  • Rogers JJW, Santosh M (2004) Continents and Supercontinents. Oxford University Press, USA, p 289p

    Google Scholar 

  • Roobol MJ, Wright JV, Smith AL (1983) Calderas or gravity-slide structures in the Lesser Antilles island arc? J Volcanol Geotherm Res 19:121–134

    Article  Google Scholar 

  • Samuel MD, Be’eri-Shlevin Y, Azer MK, Whitehouse MJ, Moussa HE (2011) Provenance of conglomerate clasts from the volcanosedimentary sequence at Wadi Rutig in Southern Sinai, Egypt as revealed by SIMS U-Pb dating of zircon. Gondwana Res 20:450–464

    Article  Google Scholar 

  • Sassi FP, Visona D, Ferrara G, Gatto GO, Ibrahim HA, Said AA, Tonarini S (1993) The crystalline basement of northern Somalia: lithostratigraphy and the sequence of events. In: Abbate E, Sagri M, Sassi FP (eds) Geology and mineral resources of Somalia and surrounding regions: relazioni e monographie agrarie subtropicali e tropicali nuova serie. Florence, Istituto Agronomico l’Otremare, pp 3–40

    Google Scholar 

  • Schandelmeier H, Darbyshire DPF, Harms U, Richter A (1988) The east Saharan Craton: evidence for pre-Pan-African crust in NE Africa west of the Nile. In: El-Gaby S, Greiling RO (eds) The Pan-African belts of Northeast Africa and adjacent areas. Vieweg & Sohn, Wiesbaden, pp 69–94

    Google Scholar 

  • Schandelmeier H, Richer A, Harms U, Abdel-Rahman EM (1990) Lithology and structure of the late Proterozoic Jebel Rahib fold-and-thrust belt (SW Sudan). Berliner Geowissen Abher (A) 120(1):15–30

    Google Scholar 

  • Shang CK, Satir M, Morteani G, Taubald H (2010) Zircon and titanite age evidence for coeval granitization and migmatization of the early Middle and early Late Proterozoic Saharan Metacraton: example from the central north Sudan basement. J Afr Earth Sci 57:492–524

    Article  Google Scholar 

  • Schulter T (1997) Geology of East Africa. Beträge zur Regionale Geologie der Erde, Band 27, Gebrüder Borntraeger, Verslagsbuchhandlung, 484 pp

    Google Scholar 

  • Schürmann HME (1966) The Precambrian Along the Gulf of Suez and the Northern Part of the Red Sea. EJ Brill, Leiden, p 404p

    Google Scholar 

  • Shimron AE (1980a) Proterozoic island arc volcanism and sedimentation in Sinai. Precambr Res 12:437–458

    Article  Google Scholar 

  • Shimron AE (1980b) Late phase deformation and mylonite belts in Sinai: Pan African thrust fault tectonics. Geol Surv Isr Curr Res 1980:75–80

    Google Scholar 

  • Shimron AE (1984a) Metamorphism and tectonism of a Pan-African terrain in southeastern Sinai—a discussion. Precambr Res 24:173–188

    Article  Google Scholar 

  • Shimron AE (1984b) Evolution of the Kid Group, southeast Sinai Peninsula: thrusts, mélanges, and implications for accretionary tectonics during the late Proterozoic of the Arabian-Nubian Shield. Geology 12:242–247

    Article  Google Scholar 

  • Shimron AE, Furnes H, Roberts D, Bogoch R (1993a) Petrogenesis of the Late Proterozoic Sa’al Group—southern Sinai Peninsula. Geol Surv Israel Curr Res 8:24–29

    Google Scholar 

  • Shimron AE, Bogoch R, Furnes H, Roberts D (1993b) The Sa’al Group: an ensialic island arc sequence in Sinai. In: Thorweihe U, Schandelmeier H (eds) Scientific research in Northeast Africa. Balkema, Rotterdam, pp 49–53

    Google Scholar 

  • Siedner G, Shimron A, Pringle JR (1974) Age relationships in basement rocks of the Sinai Peninsula: Internat. Meet., Geochron. Cosmo. Isotop. Geol., Paris (Abstract)

    Google Scholar 

  • Squire RJ, Campbell IH, Allen CM, Wilson CJL (2006) Did the Transgondwanan Supermountain trigger the explosive radiation of animals on Earth? Earth Planet Sci Lett 250:116–133

    Article  Google Scholar 

  • Stacey JS, Agar RA (1985) U-Pb isotopic evidence for the accretion of a continental micro-plate in the Zalm region of the Saudi Arabian Shield. J Geol Soc Lond 142:1189–1203

    Article  Google Scholar 

  • Stacey JS, Hedge CE (1984) Geochronologic and isotopic evidence for early Proterozoic crust in the eastern Arabian Shield. Geology 12:310–313

    Article  Google Scholar 

  • Stacey JS, Stoeser DB (1983) Distribution of oceanic and continental leads in the Arabian-Nubian Shield. Contrib Mineral Petrol 84:91–105

    Article  Google Scholar 

  • Stacey JS, Doe BR, Roberts RJ (1980) Lead isotope study of mineralization in the Saudi Arabian Shield. Contrib Mineral Petrol 74:175–188

    Article  Google Scholar 

  • Stein M, Goldstein SL (1996) From plume head to continental lithosphere in the Arabian-Nubian Shield. Nature 382:773–778

    Article  Google Scholar 

  • Stein M, Hofmann AW (1994) Mantle plumes and episodic crustal growth. Nature 372:63–68

    Article  Google Scholar 

  • Stephan T, Kröner U, Romer RL (2019a) The pre-orogenic detrital zircon record of the Peri-Gondwanan crust. Geol Mag 156:281–307

    Article  Google Scholar 

  • Stephan T, Kröner U, Romer RL, Rösel D (2019b) From a bipartite Gondwanan shelf to an arcuate Variscan belt: the early Paleozoic evolution of northern Peri-Gondwana. Earth-Sci Rev 192:491–512

    Article  Google Scholar 

  • Stern RJ (1981) Petrogenesis and tectonic setting of late Precambrian ensimatic volcanic rocks, central Eastern Desert of Egypt. Precambr Res 16:195–230

    Article  Google Scholar 

  • Stern RJ (1994) Arc assembly and continental collision in the Neoproterozoic East African Orogen: implications for the consolidation of Gondwanaland. Annu Rev Earth Planet Sci 22:319–351

    Article  Google Scholar 

  • Stern RJ (2002) Crustal evolution in the East African Orogen: a neodymium isotopic perspective. J Afr Earth Sci 34:109–117

    Article  Google Scholar 

  • Stern RJ, Hedge CE (1985) Geochronologic and isotopic constraints on late Precambrian crustal evolution in the Eastern Desert of Egypt. Am J Sci 285:97–127

    Article  Google Scholar 

  • Stern RJ, Manton WI (1987) Age of Feiran basement rocks, Sinai: implications for late Precambrian evolution in the northern Arabian-Nubian Shield. J Geol Soc Lond 144:569–575

    Article  Google Scholar 

  • Stern RJ, Kröner A, Bender R, Reischmann T, Dawoud AS (1994) Precambrian basement around Wadi Halfa, Sudan: a new perspective on the evolution of the East Saharan Craton. Geol Rundschau 83:564–577

    Article  Google Scholar 

  • Stern RJ, Johnson PR, Kröner A, Yibas B (2004) Neoproterozoic ophiolites of the Arabian-Nubian Shield. In: Kusky TM (ed) Precambrian ophiolites and related rocks. Developments in Precambr Res 13:95–128

    Google Scholar 

  • Stern RJ, Ali KA, Liegeois JP, Johnson PR, Kozdroj W, Kattan FH (2010) Distribution and significance of pre-Neoproterozoic zircons in juvenile Neoproterozoic igneous rocks of the Arabian-Nubian Shield. Am J Sci 310:791–811

    Article  Google Scholar 

  • Sultan M, Tucker RD, El Alfy Z, Attia R, Ragab A (1994) U-Pb (zircon) ages for the gneissic terrane west of the Nile, Southern Egypt. Geol Rundsch 83:514–522

    Article  Google Scholar 

  • Teklay M, Kröner A, Mezger K, Oberhänsli R (1998) Geochemistry, Pb-Pb single zircon ages and Nd-Sr isotope composition of Precambrian rocks from southern and eastern Ethiopia: implications for crustal evolution in East Africa. J Afr Earth Sci 26:207–227

    Article  Google Scholar 

  • Toteu SF, Penaye J, Djomani YP (2004) Geodynamic evolution of the Pan-African belt in Central Africa with special reference to Cameroon. Can J Earth Sci 41:73–85

    Article  Google Scholar 

  • Tretyakova AA, Kovachb VP, Shatagin KN (2016) Sources of Mesoproterozoic Igneous Rocks and Formation Time of the Continental Crust of the Kokchetav Massif (Northern Kazakhstan). Dokl Earth Sci 471–2:1312–1315

    Article  Google Scholar 

  • Vail JR (1983) Pan-African crustal accretion in NE Africa. J Afr Earth Sci 1:285–294

    Google Scholar 

  • Viola G, Henderson IHC, Bingen B, Thomas RJ, Smethurst MA, deAzavedo S (2008) Growth and collapse of a deeply eroded orogen: insights from structural, geophysical, and geochronological constraints on the Pan-African evolution of NE Mozambique. Tectonics 27, TC5009. http://dx.doi.org/10.1029/2008TC002284

  • Warden AJ, Horkel AD (1984) The Geological Evolution of the NE-Branch of the Mozambique Belt (Kenya, Somalia, Ethiopia). Mitt österr Geol Ges 77:161–184

    Google Scholar 

  • Whitehouse MJ, Windley BF, Ba-Bttat MAO, Fanning CM, Rex DC (1998) Crustal evolution and terrane correlation in the eastern Arabian Shield, Yemen: geochronological constraints. J Geol Soc Lond 155:281–295

    Article  Google Scholar 

  • Whitehouse MJ, Stoeser DB, Stacey JS (2001a) The Khida terrane geochronological and isotopic evidence for Paleoproterozoic and Archean crust in the eastern Arabian Shield of Saudi Arabia. Gondwana Res 4:200–202

    Article  Google Scholar 

  • Whitehouse MJ, Windley BF, Stoeser DB, Al-Khirbash S, Ba-Bttat MAO, Haider A (2001b) Precambrian basement character of Yemen and correlations with Saudi Araba and Somalia. Precambr Res 105:357–369

    Article  Google Scholar 

  • Windley BF, Whitehouse MJ, Ba-Bttat MAO (1996) Early Precambrian gneiss terranes and Pan-African island arcs in Yemen; crustal accretion of the eastern Arabian Shield. Geology 24:131–134

    Article  Google Scholar 

  • Yeshanew FG, Pease V, Whitehouse MJ, Al-Khirbash S (2015) Zircon U-Pb geochronology and Nd isotope systematics of the Abas terrane, Yemen: Implications for Neoproterozoic crust reworking events. Precambr Res 267:106–120

    Article  Google Scholar 

  • Yeshanew FG, Pease V, Abdelsalam MG, Whitehouse MJ (2017) Zircon U-Pb ages, δ18O and whole-rock Nd isotopic compositions of the Dire Dawa Precambrian basement, Eastern Ethiopia: Implications for the assembly of Gondwana. J Geol Soc London 174:142–156

    Article  Google Scholar 

  • Zeh A, Gerdes A, Barton JM Jr (2009) Archean accretion and crustal evolution of the Kalahari Craton—the zircon age and Hf isotope record of granitic rocks from Barberton/Swaziland to the Francistown Arc. J Petrol 50(5):933–966

    Article  Google Scholar 

  • Zhang W, Pease V, Whitehouse MJ, El-Sankary MM, Shalaby MH (2019) Pre-Neoproterozoic basement evolution of southwestern Egypt. Int Geol Rev 61(15):1909–1926

    Article  Google Scholar 

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  1. Faculty of Earth Sciences, King Abdul Aziz University, Jeddah, Saudi Arabia

    Hamdy H. Abd El-Naby

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  1. Hamdy H. Abd El-Naby
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Editors and Affiliations

  1. Department of Geology, Faculty of Science, Banha University, Benha, Egypt

    Zakaria Hamimi

  2. Department of Geology, United Arab Emirates University, Al Ain, United Arab Emirates

    Abdel-Rahman Fowler

  3. Department of Geology and Mineralogy, Royal Museum for Central Africa, Tervuren, Belgium

    Jean-Paul Liégeois

  4. Department of Earth Sciences, University of Adelaide, Adelaide, SA, Australia

    Alan Collins

  5. Boone Pickens School of Geology, Oklahoma State University, Oklahoma City, OK, USA

    Mohamed G. Abdelsalam

  6. Department of Geology, Tanta University, Tanta, Egypt

    Mohamed Abd EI-Wahed

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El-Naby, H.H.A. (2021). Evidence for Mesoproterozoic Components in the Arabian-Nubian Shield. In: Hamimi, Z., Fowler, AR., Liégeois, JP., Collins, A., Abdelsalam, M.G., Abd EI-Wahed, M. (eds) The Geology of the Arabian-Nubian Shield. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-030-72995-0_14

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