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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
    ISSN: 0016-7835
    Keywords: Key words Arabian-Nubian shield ; Continental crust ; granites ; Sraisotopes ; Nd-isotopes ; Pb-isotopes ; U-Pb zircon ages
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Major and trace element data, U–Pb zircon ages, and initial isotopic compositions of Sr, Nd, and Pb are reported for ten granitic and one rhyolitic rock sample from the neo-Proterozoic Nakasib suture in NE Sudan. Chemical data indicate that the samples are medium- to high-K, "I-type" granitic rocks that mostly plot as "volcanic arc granites" on discriminant diagrams. Geochronologic data indicate that rifting occurred 790±2 Ma and constrain the time of deformation associated with suturing of the Gebeit and Haya terranes to have ended by approximately 740 Ma. Isotopic data show a limited range, with initial 87Sr/86Sr=0.7021 to 0.7032 (mean=0.7025), εNd(t) =+5.5 to +7.0 (mean=+6.4), and 206Pb/204Pb = 17.50–17.62. Neodymium model ages (TDM; 0.69–0.85 Ga; mean = 0.76 Ga) are indistinguishable from crystallization ages (0.79–0.71 Ga; mean=0.76 Ga), and the isotopic data considered together indicate derivation from homogeneously depleted mantle. The geochronologic data indicate that the terrane accretion to form the Arabian–Nubian shield began just prior to 750 Ma. The isotopic data reinforces models for the generation of large volumes of juvenile continental crust during neo-Proterozoic time, probably at intra-oceanic convergent margins. The data also indicate that crust formation was associated with two cycles of incompatible element enrichment in granitic rocks, with an earlier cycle beginning approximately 870 Ma and culminating approximately 740 Ma, and the second cycle beginning after pervasive high-degree melts – possibly hot-spot related – were emplaced approximately 690–720 Ma.
    Type of Medium: Electronic Resource
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  • 4
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    PANGAEA
    In:  Supplement to: Njinju, Emmanuel A; Kolawole, Folarin; Atekwana, Estella A; Stamps, D Sarah; Atekwana, Eliot A; Abdelsalam, Mohamed G; Mickus, Kevin L (2019): Terrestrial heat flow in the Malawi Rifted Zone, East Africa: Implications for tectono-thermal inheritance in continental rift basins. Journal of Volcanology and Geothermal Research, 387, 106656, https://doi.org/10.1016/j.jvolgeores.2019.07.023
    Publication Date: 2023-01-13
    Description: This is the data file of the geothermal parameters which include, Curie point depth, geothermal gradient and heat flow for the Malawi Rifted Zone derived from aeromagnetic data.
    Keywords: Aeromagnetic data; Africa, Malawi; Curie point depth; geothermal gradient; Geothermal gradient; heat flow; Heat flow; LATITUDE; LONGITUDE; Malawi_rift_area; Malawi Rift; SAT; Satellite remote sensing
    Type: Dataset
    Format: text/tab-separated-values, 297 data points
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  • 5
    Publication Date: 2023-12-02
    Keywords: Africa, Malawi; gravity; LAB; LATITUDE; Lithosphere-asthenosphere boundary depth; LONGITUDE; Malawi; Malawi_rift_area; Moho; SAT; Satellite remote sensing
    Type: Dataset
    Format: text/tab-separated-values, 289 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Njinju, Emmanuel A; Atekwana, Estella A; Stamps, D Sarah; Abdelsalam, Mohamed G; Atekwana, Eliot A; Mickus, Kevin L; Fishwick, Stewart; Kolawole, Folarin; Rajaonarison, Tahiry A; Nyalugwe, Victor N (2019): Lithospheric Structure of the Malawi Rift: Implications for Magma‐Poor Rifting Processes. Tectonics, 38(11), 3835-3853, https://doi.org/10.1029/2019TC005549
    Publication Date: 2023-12-02
    Description: The data files contain the depth to Moho and depth to LAB beneath the Malawi Rift and surroundings generated from spectral analysis of WGM2012 Bouguer gravity anomalies. Latitude (degree), longitude (degree) and depth (km).
    Keywords: Africa, Malawi; gravity; LAB; Malawi; Malawi_rift_area; Moho; SAT; Satellite remote sensing
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    Publication Date: 2023-12-02
    Keywords: Africa, Malawi; gravity; LAB; LATITUDE; LONGITUDE; Malawi; Malawi_rift_area; Moho; Mohorovicic Discontinuity depth; SAT; Satellite remote sensing
    Type: Dataset
    Format: text/tab-separated-values, 289 data points
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  • 8
    Publication Date: 2012-03-01
    Description: Magnetic stripes parallel to mid-ocean ridges are one of the most significant consequences of seafloor spreading, and have played an essential role in the establishment of the plate tectonics theory and the determination of seafloor spreading rates. Similar magnetic anomaly patterns have not been well documented subaerially in continental rifts transitioning into seafloor spreading centers. Here, using high-resolution magnetic data that were collected across the Tendaho Graben in the Afar Depression, Ethiopia, we document one of the first examples of subaerial magnetic lineations similar in pattern and amplitude to those that characterize seafloor spreading centers. The ~50-km-wide graben is the southernmost structural and geomorphological expression of the on-land continuation of the Red Sea propagator, which is taken to represent the Arabian-Nubian plate boundary within Afar. The graben is bounded by northwest-trending border faults, with the footwalls dominated by ca. 1.7 Ma basalts and the downthrown blocks constituting progressively younger basalts toward the center of the graben, reaching ca. 35 ka. The Tendaho magnetic field is characterized by an ~10-km-wide linear negative magnetic anomaly that corresponds to a normal-polarity zone that is flanked by two parallel, ~20-km-wide linear positive magnetic anomalies of reversed polarity. This work shows that magnetic stripes can be developed in transitional continental rifts before the development of oceanic spreading centers. The common assumption that magnetic stripes can be used to date the onset of seafloor spreading may need to be re-evaluated in light of the evidence provided here.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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