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  • 1
    Online Resource
    Online Resource
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Keywords: Physical geography. ; Earth sciences. ; Remote sensing. ; Ägypten Nord ; Nubischer Schild ; Ostafrikanisches Orogen ; Oberproterozoikum ; Kollisionsorogenese ; Metamorphes Ergussgestein ; Nubischer Schild ; Erzlagerstätte ; Proterozoikum ; Metallogenese ; Bändereisenerz ; Ägypten ; Ophiolith ; Ophiolithkomplex ; Goldlagerstätte ; Sutur ; Lagerstättenbildung ; Vulkanisch-sedimentäres Gestein ; Vulkanismus ; Geologie ; Tektonik ; VHMS-Lagerstätte ; Lagerstättenkunde ; Sudan ; Schild ; Erzlagerstätte ; Vorkommen ; Kupferlagerstätte
    Description / Table of Contents: 1. The Arabian-Nubian Shield, an introduction: historic overview, concepts, interpretations, and future issues -- 2. The boundary between the Saharan metacraton and the Arabian Nubian Shield: insight from Ediacaran shoshonitic granites of the Nuba Mountains (Sudan): U–Pb SHRIMP zircon dating, geochemistry and Sr-Nd isotope constraints -- 3. The Southern Part of the Arabian Nubian Shield in Kenya and Tanzania Harald Fritz and Christoph Hauzenberger -- 4. Tectonic Evolution of the Pan-African Belt in Western Ethiopia, Southern Arabian-Nubian Shield -- 5. Neoproterozoic Crustal Evolution of the northernmost Arabian-Nubian Shield, south Jordan.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXIX, 771 p. 399 illus., 365 illus. in color.)
    Edition: 1st ed. 2021.
    ISBN: 9783030729950
    Series Statement: Regional Geology Reviews
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Geology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (786 pages)
    Edition: 1st ed.
    ISBN: 9783030729950
    Series Statement: Regional Geology Reviews Series
    Language: English
    Note: Intro -- Preface -- Why This Book? -- Contents -- Contents -- About the Editors -- 1 The Arabian-Nubian Shield, an Introduction: Historic Overview, Concepts, Interpretations, and Future Issues -- Abstract -- 1.1 Introduction -- 1.2 ANS: Plate Tectonic Setting -- 1.3 ANS: Geologic Investigations -- 1.3.1 Historic Developments -- 1.3.2 Mineral Resources and Exploration -- 1.3.3 Geologic Mapping, Surveys, and Findings -- 1.4 ANS: Nomenclature -- 1.5 ANS: External Boundaries -- 1.5.1 ANS Northwestern Margin -- 1.5.2 ANS Southern Margin -- 1.5.3 ANS Eastern Margin -- 1.5.4 ANS Margins in the Southwestern Arabian Peninsula -- 1.5.5 ANS Margins in the Eastern Arabian Peninsula -- 1.5.6 ANS Northern Extent -- 1.6 ANS: Internal Divisions -- 1.6.1 Volcanic Arcs -- Where, How Many, and Origin? -- 1.6.2 Mineral Belts: An Aid to Metallogenic Analysis and Exploration Targeting -- 1.6.3 Structural or Tectonic Belts and Domains -- 1.6.4 Divisions in the Egyptian Eastern Desert -- 1.6.5 Tectonostratigraphic Terranes -- 1.6.6 Isotopic Domains -- 1.6.7 Inherited Zircons -- 1.7 Concluding Comments -- Acknowledgements -- References -- 2 The Boundary Between the Saharan Metacraton and the Arabian Nubian Shield: Insight from Ediacaran Shoshonitic Granites of the Nuba Mountains (Sudan): U-Pb SHRIMP Zircon Dating, Geochemistry and Sr-Nd Isotope Constraints -- Abstract -- 2.1 Introduction -- 2.2 Granitoids in the ANS and the SmC and Change in Stress Regime -- 2.3 The SmC-ANS Boundary in Sudan -- 2.4 Geological Setting and Petrography -- 2.5 U-Pb SHRIMP Dating of Zircon -- 2.5.1 Analytical Techniques -- 2.5.2 Results -- 2.6 Geochemistry of the Late-Orogenic Granitoids -- 2.6.1 Analytical Techniques -- 2.6.2 Major and Trace Elements Chemistry -- 2.7 Sr and Nd Isotopes -- 2.7.1 Analytical Techniques -- 2.7.2 Rb-Sr and Sm-Nd Isotopic Results -- 2.8 Discussion. , 2.8.1 Lithochemistry and Structural Characterization of the Nuba Post-collisional Plutons -- 2.8.2 The Source of the Parental Magma of the Nuba Post-collisional Plutons -- 2.8.3 Timing of Magmatism, Metamorphism and Regional Correlations -- 2.8.4 Implications for the Boundary of the Saharan Metacraton in Southern Sudan -- 2.9 Conclusions -- Acknowledgements -- References -- 3 The Southern Part of the Arabian-Nubian Shield in Kenya and Tanzania -- Abstract -- 3.1 Introduction -- 3.2 Geological Overview -- 3.3 Lithology, Formation Ages and Tectonic Setting -- 3.3.1 Sobo Unit -- 3.3.2 Galana Unit -- 3.3.3 Sagala Unit -- 3.3.4 Kinyjki Unit/Kasigau Group -- 3.3.5 Kurase Group/Eastern Granulites Metasediments -- 3.3.6 Eastern Granulites Metamagmatics -- 3.4 Isotopic Constraints -- 3.5 Tectonics and Metamorphism -- 3.6 Interpretation -- 3.7 Discussion and Conclusions -- Acknowledgements -- References -- 4 Tectonic Evolution of the Pan-African Belt in Western Ethiopia, Southern Arabian-Nubian Shield -- Abstract -- 4.1 Introduction -- 4.2 Regional Geologic Setting -- 4.3 Lithology -- 4.3.1 Gimbi Terrane -- 4.3.2 Nejo Terrane -- 4.3.3 Asosa Terrane -- 4.3.4 Tulu Dimtu-Baruda Belt -- 4.3.5 Intrusive Rocks -- 4.3.6 Young Volcano-Sediments -- 4.4 Structures -- 4.4.1 Gimbi Terrane -- 4.4.2 Nejo Terrane -- 4.4.3 Asosa Terrane -- 4.4.4 Tulu Dimtu-Baruda Belt -- 4.4.5 NW-Trending Structures -- 4.5 Discussion and Summary -- 4.5.1 Structural Evolution -- 4.5.2 Tectonic Interpretation and Regional Correlation of Terranes -- Acknowledgements -- References -- 5 Neoproterozoic Crustal Evolution of the Northernmost Arabian-Nubian Shield, South Jordan -- Abstract -- 5.1 Introduction -- 5.2 Aqaba Complex -- 5.2.1 Metamorphic Suites -- 5.2.1.1 Abu Barqa Metamorphic Suite -- 5.2.1.2 Janub Metamorphic Suite (JMS) -- 5.2.1.3 Abu Saqa Schist -- 5.2.2 Gabbroids and Granitoids. , 5.2.2.1 Duheila Hornblendic Suite (DHS) -- 5.2.2.2 Rahma Foliated Suite (RFS) -- 5.2.2.3 Darba Tonalitic Suite -- 5.2.2.4 Urf Porphyritic Suite (UPS) -- 5.2.2.5 Rumman Suite (RS) -- 5.2.2.6 Yutum Suite (YS) -- 5.3 Araba Complex -- 5.3.1 Safi Group -- 5.3.1.1 Saramuj Conglomerate Formation (SCF) -- 5.3.1.2 Haiyala Volcaniclastic Formation (HVF) -- 5.3.2 The Araba Mafic Suite -- 5.3.3 Humrat-Feinan-Mubarak Suite (HFMS) -- 5.3.4 Aheimir Volcanic Suite (AVS) -- 5.4 Ediacaran Dike Swarms -- 5.5 Summary and Conclusions -- Acknowledgements -- References -- 6 Lithospheric Structure of the Arabian-Nubian Shield Using Satellite Potential Field Data -- Abstract -- 6.1 Introduction -- 6.2 Data -- 6.3 Methodology -- 6.3.1 EHGA Method -- 6.3.2 Parker-Oldenburg Method -- 6.4 Results -- 6.4.1 Edge Results -- 6.4.2 Moho and LAB Results -- 6.5 Discussion -- 6.6 Conclusions -- Acknowledgements -- References -- 7 Evolution of the Arabian Nubian Shield and Snowball Earth -- Abstract -- 7.1 Introduction -- 7.2 Snowball Earth and Late Neoproterozoic Glaciation -- 7.3 Overview of ANS and EAO Development -- 7.4 Expected Manifestations of Neoproterozoic Glaciations in the ANS and EAO -- 7.5 Evidence for Glaciation in the ANS -- 7.5.1 Evidence for Tonian (c. 780-755 Ma) Glaciation -- 7.5.1.1 sim780 Ma Diamictite in Eastern Sudan (Meritri Group) and Central Arabian Shield (Mahd Group) -- 7.5.1.2 sim750 Ma Ghamr and Amudan Volcanosedimentary Basins, Central Arabian Shield -- 7.5.2 Evidence for Sturtian Glaciation (sim717-659 Ma) -- 7.5.2.1 Ethiopia/Eritrea-Tambien Group -- 7.5.2.2 Banded Iron Formation of Egypt and Arabia -- 7.5.2.3 Atud Diamictite (Egypt) and Nuwaybah Formation (Zaam Group) (NW Arabia) -- 7.5.2.4 Um Zariq and Zaghara Formations, Sinai Peninsula, Egypt, Northern ANS -- 7.5.2.5 Hadiyah Group, NW Arabian Shield. , 7.5.3 Evidence for Marinoan (Onset sim650-639, to sim635 Ma) and Ediacaran (sim580-550 Ma) Glaciation -- 7.5.3.1 Post-amalgamation (Ediacaran) Basins -- 7.5.3.2 Gondwanan Margin Basins -- 7.5.3.3 Role of Glaciation in the Formation of the Afro-Arabian Peneplain -- 7.6 Conclusions -- Acknowledgements -- References -- 8 The Arabian-Nubian Shield Within the Neoproterozoic Plate Tectonic Circuit -- Abstract -- 8.1 Introduction -- 8.2 A Full-Plate Tectonic Reconstruction -- 8.3 The ANS Within the Northern 'East African Orogen' -- 8.4 The Mozambique Ocean, Azania and Afif-Abas -- 8.5 The Eastern Margin of the EAO (NW India to Oman) -- 8.6 The Arabian-Nubian Shield (ANS) -- 8.7 The Western Margin of the EAO (the Eastern Saharan Metacraton) -- 8.8 Discussion -- 8.9 Conclusions -- Acknowledgements -- References -- 9 Early Ensimatic Stage of the Arabian-Nubian Shield -- Abstract -- 9.1 Introduction -- 9.2 Rodinia Pre-rifting Configurations -- 9.2.1 SWEAT Model -- 9.2.2 "Missing-Link" Model -- 9.2.3 Other Models -- 9.3 Rodinia Rifting -- 9.4 Origins and Configurations of the Mozambique Ocean-Rift or Remnant? -- 9.5 Remnants of Rodinia Within the ANS -- 9.5.1 Rodinia Continental Signatures Within the ANS -- 9.5.2 Mozambique Ocean Signatures Within the ANS -- 9.5.2.1 Setting and Occurrence -- 9.5.2.2 Magma Type -- 9.5.2.3 Tectonic Setting -- 9.6 Conclusions and Open Questions -- References -- 10 Terrane Accretion Within the Arabian-Nubian Shield -- Abstract -- 10.1 Introduction -- 10.2 The Rationale -- 10.2.1 Terrane Terminology -- 10.2.2 Formation of Terranes -- 10.3 Formation and Amalgamation of Gondwana Supercontinent -- 10.3.1 Neoproterozoic Pan-African Orogeny -- 10.3.2 The East African Orogen (EAO) -- 10.4 The Arabian-Nubian Shield (ANS) -- 10.4.1 Terrane Analysis, Amalgamation, and Accretion of the ANS -- 10.4.2 Assembly of the ANS and Crustal Growth. , 10.5 Tectonic Models of the ANS -- 10.5.1 Earlier Models of Evolution of ANS -- 10.5.1.1 A Single Immature Island Arc Evolution (Island Arc-Accretion Model) -- 10.5.1.2 Successive Formation and Accretion of Ensimatic Island Arcs Model -- 10.5.1.3 Repeated Rifting of an Older Sialic Crust -- 10.5.1.4 Microplate Accretion Model -- 10.5.1.5 Reconstruction of the ANS Model -- 10.5.1.6 Pan-African Continental Margin Model -- 10.5.2 Recent Models of ANS Evolution: Arc-Accretion Model -- 10.6 Faults and Shear Zones in the ANS -- 10.7 Ophiolite Zones as Evidence for Sutures in the ANS -- 10.7.1 Arc-Arc Sutures -- 10.7.2 Arc-Continent Sutures -- 10.7.3 The Eastern Margin of the ANS -- 10.7.4 The Western Margin of the ANS -- 10.8 Post-accretionary Structures -- 10.9 Post-amalgamation Basins of the NE Arabian Shield -- 10.10 Conclusions -- References -- 11 Tonian/Cryogenian Island Arc Metavolcanics of the Arabian-Nubian Shield -- Abstract -- 11.1 Introduction -- 11.2 Island Arc Volcanism of the Northern Nubian Shield -- 11.2.1 Island Arc Volcanic Rocks of the Eastern Desert of Egypt -- 11.2.1.1 Island Arc Volcanic Rocks of North Eastern Desert (NED) -- 11.2.1.2 Island Arc Volcanic Rocks of Central Eastern Desert (CED) -- 11.2.1.3 Island Arc Volcanic Rocks of South Eastern Desert (SED) -- 11.2.1.4 Mineralization Related to Island Arc Volcanism of the Eastern Desert of Egypt -- 11.2.1.5 Age of the Younger Metavolcanic Rocks of the Eastern Desert -- 11.2.2 Island Arc Volcanic Rocks of Sinai -- 11.2.3 Geochemistry and Petrogenesis of Island Arc Volcanics in the Eastern Desert of Egypt -- 11.2.3.1 Geochemical Characters of Major, Trace and REEs -- 11.2.3.2 Tectonomagmatic Discrimination Plots -- 11.2.3.3 Petrogenesis -- (i) Tholeiitic Metavolcanics -- (ii) Calc-Alkaline Metavolcanics -- (iii) Felsic Metavolcanics. , 11.2.3.4 Stages of Island Arc Volcanicity in the Eastern Desert.
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  • 3
    Keywords: Cratons ; Westafrika ; Kraton
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (VIII, 533 Seiten)
    ISBN: 9781862392519
    Series Statement: Geological Society special publication 297
    DDC: 551.8
    RVK:
    Language: English
    Note: The boundaries of the West African craton, with special reference to the basement of the Moroccan metacratonic Anti-Atlas belt / N. Ennih & J.-P. Liégeois -- THE PALAEOPROTEROZOIC TERRANES FROM THE WEST AFRICAN CRATON AND THEIR REWORKING: REE patterns, Nd-Sm and U-Pb ages of the metamorphic rocks of the Diagorou-Darbani greenstone belt (Liptako, SW Niger): implication for Birimian (Palaeoproterozoic) crustal genesis / A. Soumaila ... [et al.] -- Two Mesoarchaean terranes in the Reguibat shield of NW Mauritania / R.M. Key ... [et al.] -- Geological setting of the Guelb Moghrein Fe oxide-Cu-Au-Co mineralization, Akjoujt area, Mauritania / J. Kolb ... [et al.] -- Possible primary sources of diamond in the North African diamondiferous province / M. Kahoui, Y. Mahdjoub & F.V. Kaminsky -- Geochronology and metamorphic P-T-X evolution of the Eburnean granulite- facies metapelites of Tidjenouine (Central Hoggar, Algeria): witness of the LATEA metacratonic evolution / A. Bendaoud ... [et al.] -- First report of ultrahightemperature sapphirine + spinel + quartz and orthopyroxene + spinel + quartz parageneses discovered in Al-Mg granulites from the Khanfous area (In Ouzzal metacraton, Hoggar, Algeria) / Z. Adjerid ... [et al.] --
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  • 4
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    Geolocigal Society London
    In:  In: The Boundaries of the West African Craton. , ed. by Ennih, N. and Liegeois, J. P. Geological Society London Special Publications, 297 . Geolocigal Society London, London, 1.1-17.
    Publication Date: 2020-08-03
    Description: The West African craton (WAC) was constructed during the Archaean and the c. 2G a Palaeoproterozoic Eburnian orogeny. Mesoproterozoic quiescence at c. 1.7-1.0 Ga allowed cratonization. In the absence of Mesoproterozoic activity, there are no known WAC palaeogeo- graphical positions for that time. At the beginning of the Neoproterozoic, the WAC was affected by several extensional events suggesting that it was subjected to continental breakup. The most important event is the formation of the Gourma aulacogen in Mali, and the Taoudeni cratonic sub- circular basin and deposition of platform sediments in the Anti-Atlas. At the end of the Neopro- terozoic, the WAC was subjected to convergence on all its boundaries, from the north in the Anti-Atlas, to the east along the Trans-Saharan belt, to the south along the Rockelides and the Bassarides and to the east along the Mauritanides. This led to a partial remobilization of its cratonic boundaries giving rise to a metacratonic evolution. The WAC boundaries experienced Pan-African Neoproterozoic to Early Cambrian transpression and transtension, intrusion of granitoids and extrusion of huge volcanic sequences in such as in the Anti-Atlas (Ouarzazate Supergroup). Pan-African tectonism generated large sediment influxes around the WAC within the Peri-Gondwanan terranes whose sedimentary sequences are marked by distinctive zircon ages of 1.8- 2.2 Ga and 0.55-0.75 Ga. WAC rocks experienced Pan-African low grade metamorphism and large movements of mineralizing fluids. In the Anti-Atlas, this Pan-African metacratonic evolution led to remobiliza- tion of REE in the Eburnian granitoids due to the activity of F-rich fluids linked to extrusion of the Ouarzazate Supergroup. During the Phanerozoic, the western WAC boundary was subjected to the Variscan orogeny, for which it constituted the foreland and was, therefore moderately affected, showing typical thick-skin tectonics in the basement and thin-skin tectonics in the cover. During the Mesozoic, the eastern and southern boundaries of the WAC were subjected to the Atlantic opening including Jurassic dolerite intrusion and capture of its extreme southern tip by South America. The Jurassic is also marked by the development of rifts on its eastern and northern sides (future Atlas belt). Finally, the Cenozoic period was marked by the convergence of the African and European continents, generating the High Atlas range and Cenozoic volcanism encir- cling the northern part of the WAC. The northern metacratonic boundary of the WAC is currently uplifted, forming the Anti-Atlas Mountains. The boundaries of the WAC, metacratonized during the Pan-African orogeny have been period- ically rejuvenated. This is a defining characteristic of the metacratonic areas: rigid, stable cratonic regions that can be periodically cut by faults and affected by magmatism and hydrothermal altera- tion - making these areas important for mineralization.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 5
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    Unknown
    Elsevier
    In:  Journal of African Earth Sciences, 112, Part B . pp. 377-381.
    Publication Date: 2019-08-28
    Type: Article , PeerReviewed
    Format: text
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