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  • 1
    Online-Ressource
    Online-Ressource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Schlagwort(e): Geochemistry. ; Electronic books.
    Beschreibung / Inhaltsverzeichnis: Final Report of the IGCP Project No. 92 (Archean Geo- chemistry).
    Materialart: Online-Ressource
    Seiten: 1 online resource (298 pages)
    Ausgabe: 1st ed.
    ISBN: 9783642700019
    DDC: 551.712
    Sprache: Englisch
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  • 2
    Online-Ressource
    Online-Ressource
    Amsterdam :Elsevier Science & Technology,
    Schlagwort(e): Plate tectonics. ; Geology, Stratigraphic -- Precambrian. ; Electronic books.
    Beschreibung / Inhaltsverzeichnis: Precambrian Plate Tectonics.
    Materialart: Online-Ressource
    Seiten: 1 online resource (805 pages)
    Ausgabe: 1st ed.
    ISBN: 9780080869032
    Serie: Issn Series ; v.Volume 4
    DDC: 551.71
    Sprache: Englisch
    Anmerkung: Front Cover -- Precambrian Plate Tectonics -- Copyright Page -- Contents -- Foreword -- Introduction -- Contributing Authors -- Part 1: General reviews of Precambrian crustal evolution -- CHAPTER 1. PRECAMBRIAN ROCKS IN THE LIGHT OF THE PLATE- TECTONIC CONCEPT -- Abstract -- Introduction -- The heat factor -- Palaeomagnetism -- Archaean crustal evolution -- Early-mid-Proterozoic geosynclines, mobile belts and plate collisions -- Mid-Proterozoic rifting and magmatism -- Grenville-Dalslandian mobile belt -- The Pan-African-Braziliano mobile belts -- Precambrian plate tectonics -- References -- CHAPTER 2. PRECAMBRIAN TECTONIC STYLE: A LIBERAL UNIFORMITARIAN INTERPRETATION -- Abstract -- Introduction -- Major uncertainties in Precambrian synthesis -- Thermal history of the earth -- Continental accretion -- Precambrian tectonic style -- Constraining assumptions -- Contemporary geodynamics -- Scale of mantle convection -- Heat flow -- Plate-driving force -- Buoyancy -- Implications for the Precambrian -- Buoyancy-powered plate tectonics -- Subduction by viscous drag -- Evolution of the protocrust -- Onset of negative buoyancy -- Intracontinental orogeny -- Crustal thickening -- Summary -- Geologic evidence -- Pre-Archaean -- Archaean -- Proterozoic -- Commentary -- Acknowledgements -- References -- CHAPTER 3. PRECAMBRIAN PLATE TECTONICS -- Abstract -- Introduction. -- The Archaean (> -- 2.5 Ga) -- Archaean plate tectonics - dominance of rifting and sag-subduction. -- The Lower Proterozoic (2.5-1.2 Ga). -- Lower Proterozoic plate tectonics-dominance of A-subduction and intraplate shearing -- The Upper Proterozoic (1.2 - 0.6 Ga) -- Upper Proterozoic tectonics - transition to contemporary plate interaction -- Conclusions -- Acknowledgements -- References -- CHAPTER 4. UNIFORMITARIAN ASSUMPTIONS, PLATE TECTONICS AND THE PRECAMBRIAN EARTH -- Abstract. , The uniformitarian doctrine -- Methodological problems in earth science. -- Possible relevance of plate tectonics to Precambrian history. -- Ophiolites -- Two-stage mantle melting products. -- Lateral accretion. -- Palaeomagnetic evidence and Precambrian geotectonics -- Temporally unique Precambrian features -- Acknowledgements -- References. -- Part 2: Archaean tectonics -- CHAPTER 5. ARCHAEAN PLATES AND GREENSTONE BELTS -- Abstract -- Introduction. -- Greenstone belts. -- Peninsular India -- Setting -- Lithostratigraphy -- Geochronology -- Tectonic development -- Southern Africa: Rhodesian and Kaapvaal cratons -- Setting -- Lithostratigraphy -- Geochronology -- Tectonic development -- Western Australia: Yilgarn subprovince -- Setting -- Lithostratigraphy -- Geochronology -- Tectonic development -- Canadian Shield: southern Superior Province -- Setting -- Lithostratigraphy -- Geochronology -- Tectonic development -- Summary -- Archaean plates -- References -- CHAPTER 6. GEOTECTONIC EVOLUTION OF THE ARCHAEAN SUCCESSIONS IN THE BARBERTON MOUNTAIN LAND, SOUTH AFRICA -- Abstract -- Introduction -- The primordial earth's crust -- The Archaean crust of southern Africa -- The Barberton Mountain Land -- Towards an evolutionary model -- Summary -- Acknowledgements -- References -- CHAPTER 7. THE EVOLUTION OF THE RHODESIAN CRATON AND ADJACENT ARCHAEAN TERRAIN: TECTONIC MODELS -- Abstract -- Introduction -- Stratigraphic summary -- Relationship between the Rhodesian craton and the Limpopo mobile belt -- Constraints on tectonic models -- Tectonic models -- Conclusions -- Acknowledgements -- References -- CHAPTER 8. THE TECTONIC DEVELOPMENT OF THE LIMPOPO MOBILE BELT AND THE EVOLUTION OF THE ARCHAEAN CRATONS OF SOUTHERN AFRICA1 -- Abstract -- Introduction -- The Limpopo Mobile Belt -- Morphology and lithology -- Gravity and magnetic character -- Metamorphism. , Deformational history -- Chronology -- A plate-tectonic model -- Implications for crustal evolution of southern Africa -- Conclusion -- Acknowledgements -- References -- CHAPTER 9. ARCHAEAN BASIN EVOLUTION IN THE SLAVE PROVINCE, CANADA -- Abstract -- Introduction -- The Slave Structural Province -- Supracrustal rocks-the Yellowknife Supergroup -- Volcanic rocks -- Sedimentary rocks -- Basement -- Geochronology -- Origin and extent of Yellowknife supracrustal basins -- Evidence of plate tectonics in the Slave Province during the Archaean -- Acknowledgements -- References -- CHAPTER 10. TECTONICS AND PETROGENESIS OF EARLY PRECAMBRIAN COMPLEXES OF THE ALDAN SHIELD, SIBERIA -- Abstract -- Introduction -- Stratigraphy -- Gneiss-granulite basement -- Greenstone and schist belts -- Geochronology -- Petrogenesis -- Tectonics -- Crustal development -- Conclusions -- References -- Part 3: Lower to middle Proterozoic tectonics -- CHAPTER 11. PROTEROZOIC CHRONOLOGY AND EVOLUTION OF THE MIDCONTINENT REGION, NORTH AMERICA -- Abstract -- Introduction -- Geochronologic data -- Continental and tectonic setting -- Early Proterozoic terranes (2500-1600 Ma) -- Penokean region -- Archaean basement -- Pre-Penokean Proterozoic rocks -- Penokean orogenic rocks -- Post-Penokean rocks -- Western United States -- Midcontinent region -- Middle Proterozoic rocks of the midcontinent -- Undeformed plutonic rocks -- Granite-rhyolite terrane of the south-central United States -- Discussion -- Regional correlations of early Proterozoic terranes -- Origin of the early Proterozoic orogenic belts -- Origin of the middle Proterozoic granite-rhyolite terrane and undeformed plutons -- Conclusions -- Acknowledgements -- References -- CHAPTER 12. THE CIRCUM-SUPERIOR BELT: A PROTEROZOIC PLATE MARGIN? -- Abstract -- Introduction -- Elements of the Cirum-Superior Belt -- General. , Labrador Trough -- Southern Labrador Trough -- The Mistassini-Otish Groups -- The Cape Smith Belt -- The Belcher Basin -- Sutton Inlier -- The Fox River Belt -- Thompson Nickel Belt -- Molson Dykes -- Lake Superior Association -- Correlation within the Circum-Superior Belt -- General -- Stratigraphic relationships -- Magmatic relationships -- Tectonic considerations -- Conclusions -- Acknowledgements -- References -- CHAPTER 13. LABRADOR GEOSYNCLINE: TYPE EXAMPLE OF EARLY PROTEROZOIC CRATONIC REACTIVATION -- Abstract -- Introduction -- The geosynclinal filling -- Sedimentary environments and provenance -- Volcanic rocks -- Structure and metamorphism -- Autochthonous position of basalts -- Discussion -- Acknowledgements -- References -- CHAPTER 14. A GRENVILLIAN MODEL OF PROTEROZOIC PLATE TECTONICS -- Abstract -- Introduction -- Plate tectonics and subduction -- Definitions -- A choice of models -- An overview of the Grenvillian Belt -- Pre-Grenvillian Proterozoic history -- Grenvillian history and isotopic dating -- Geophysics can help -- Tectonics of Grenvillian surroundings -- A Grenvillian model -- The failure of Phanerozoic models -- Stress-fields of Proterozoic plates -- Palaeomagnetic wanderings -- Three Grenvillian stress-fields -- Mobile plates or changing fields? -- Proterozoic tectonics and a Grenvillian Tibet -- Conclusion -- Acknowledgements -- References -- Part 4: Upper Proterozoic to Lower Palaeozoic tectonics (Pan-African event) -- CHAPTER 15. PAN-AFRICAN (UPPER PROTEROZOIC) PLATE TECTONICS OF THE ARABIAN-NUBIAN SHIELD -- Abstract -- Introduction -- Field, petrographic and geochemical data -- Lower Pan-African -- Middle Pan-African -- Upper Pan-African -- Plate-tectonic considerations -- Acknowledgements -- References -- CHAPTER 16. PAN-AFRICAN CLOSURE AND CONTINENTAL COLLISION IN THE HOGGAR-IFORAS SEGMENT, CENTRAL SAHARA -- Abstract. , Introduction -- Contrasting pre-Pan-African history of the West African craton and the Touareg shield -- Early Pan-African rifting during the Upper Proterozoic -- Development of a passive continental margin -- Magmatism associated with continental fragmentation -- Initiation of ocean closure and subduction: Cordilleran-type evolution of the Pharusian belt -- Multistage structural development of the Pan-African Touareg shield -- The "Kibaran" event (1200-900 Ma ago) -- The event around 725 Ma ago -- The event around 700-680 Ma ago -- Pan-African collision of the West African craton with the Touareg shield around 600Ma AGo -- The suture -- Foreland nappes west of the suture -- Paired metamorphic belts -- Deformation in the Pharusian belt east of the suture -- Reactivation of the polycyclic central Hoggar-Aïr domain and the Tiririne linear intracontinental belt -- Conclusion -- Acknowledgements -- References -- CHAPTER 17. THE LATE PROTEROZOIC OPHIOLITES OF BOU AZZER (MOROCCO): EVIDENCE FOR PAN-AFRICAN PLATE TECTONICS -- Abstract -- Introduction -- The Bou Azzer ophiolitic complex -- Regional geology -- The Bou Azzer mafic-ultramafic complex -- Evidence for ophiolites at Bou Azzer -- Tectonic setting of the Bou Azzer ophiolite -- Discussion -- Spreading of ocean crust at Bou Azzer -- Bou Azzer ocean closing -- Conclusion -- Acknowledgements -- References -- Part 5: Geochemistry, isotope geology, petrology and geophysics: Constraints and models for Precambrian crustal evolution -- CHAPTER 18. EARTH TECTONICS AND THERMAL HISTORY: REVIEW AND A HOT-SPOT MODEL FOR THE ARCHAEAN -- Abstract -- Introduction -- Geophysical and geochemical models -- The heat flow and heat generation problem -- A hot-spot model -- Conclusion -- References -- CHAPTER 19. PETROGENESIS OF ARCHAEAN ULTRAMAFIC MAGMAS AND IMPLICATIONS FOR ARCHAEAN TECTONICS -- Abstract -- Introduction. , Quench-textured peridotites.
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  • 3
    ISSN: 1525-1314
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: New data on the metamorphic petrology and zircon geochronology of high-grade rocks in the central Mozambique Belt (MB) of Tanzania show that this part of the orogen consists of Archean and Palaeoproterozoic material that was structurally reworked during the Pan-African event. The metamorphic rocks are characterized by a clockwise P–T path, followed by strong decompression, and the time of peak granulite facies metamorphism is similar to other granulite terranes in Tanzania. The predominant rock types are mafic to intermediate granulites, migmatites, granitoid orthogneisses and kyanite/sillimanite-bearing metapelites. The meta-granitoid rocks are of calc-alkaline composition, range in age from late Archean to Neoproterozoic, and their protoliths were probably derived from magmatic arcs during collisional processes. Mafic to intermediate granulites consist of the mineral assemblage garnet–clinopyroxene–plagioclase–quartz–biotite–amphibole ± K-feldspar ± orthopyroxene ± oxides. Metapelites are composed of garnet-biotite-plagioclase ± K-feldspar ± kyanite/sillimanite ± oxides. Estimated values for peak granulite facies metamorphism are 12–13 kbar and 750–800 °C. Pressures of 5–8 kbar and temperatures of 550–700 °C characterize subsequent retrogression to amphibolite facies conditions. Evidence for a clockwise P–T path is provided by late growth of sillimanite after kyanite in metapelites. Zircon ages indicate that most of the central part of the MB in Tanzania consists of reworked ancient crust as shown by Archean (c. 2970–2500 Ma) and Palaeoproterozoic (c. 2124–1837 Ma) protolith ages. Metamorphic zircon from metapelites and granitoid orthogneisses yielded ages of c. 640 Ma which are considered to date peak regional granulite facies metamorphism during the Pan-African orogenic event. However, the available zircon ages for the entire MB in East Africa and Madagascar also document that peak metamorphic conditions were reached at different times in different places. Large parts of the MB in central Tanzania consist of Archean and Palaeoproterozoic material that was reworked during the Pan-African event and that may have been part of the Tanzania Craton and Usagaran domain farther to the west.
    Materialart: Digitale Medien
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  • 4
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 23 (2005), S. 0 
    ISSN: 1525-1314
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: A structural, metamorphic and geochronological study of the Staré Město belt implies the existence of two distinct metamorphic events of similar peak P–T conditions (700–800 °C, 8–10 kbar) during the Cambro-Ordovician and the Carboniferous tectonometamorphic events. The hypothesis of two distinct periods of metamorphism was suggested on the basis of structural discordance between an undoubtedly Carboniferous granodiorite sill intrusion and earlier Cambro-Ordovician fabrics of a banded amphibolite complex. The analysis of crystal size distribution (CSD) shows high nucleation density (N0) and low average growth rate (Gt) for Carboniferous mylonitic metagabbros and mylonitic granodiorites. The parameter N0 decreases whereas the quantity Gt increases towards higher temperatures progressively approaching the values obtained from the Cambro-Ordovician banded amphibolite complex. The spatial distribution of amphibole and plagioclase shows intense mechanical mixing for lower-temperature mylonitic metagabbros. In high-temperature mylonites a strong aggregate distribution is developed. Cambro-Ordovician amphibolites unaffected by Carboniferous deformation show a regular to anticlustered spatial distribution resulting from heterogeneous nucleation of individual phases. This pattern, together with CSD, was subsequently modified by the grain growth and textural equilibration controlled by diffusive mass transfer during Carboniferous metamorphism. The differences between the observed textures of the amphibolites are interpreted to be a consequence of the different durations of the Carboniferous and Cambro-Ordovician thermal events.
    Materialart: Digitale Medien
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  • 5
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 20 (2002), S. 0 
    ISSN: 1525-1314
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: SHRIMP U–Pb ages have been obtained for zircon in granitic gneisses from the aureole of the Rogaland anorthosite–norite intrusive complex, both from the ultrahigh temperature (UHT; 〉900 °C pigeonite-in) zone and from outside the hypersthene-in isograd. Magmatic and metamorphic segments of composite zircon were characterised on the basis of electron backscattered electron and cathodoluminescence images plus trace element analysis. A sample from outside the UHT zone has magmatic cores with an age of 1034 ± 7 Ma (2σ, n = 8) and 1052 ± 5 Ma (1σ, n = 1) overgrown by M1 metamorphic rims giving ages between 1020 ± 7 and 1007 ± 5 Ma. In contrast, samples from the UHT zone exhibit four major age groups: (1) magmatic cores yielding ages over 1500 Ma (2) magmatic cores giving ages of 1034 ± 13 Ma (2σ, n = 4) and 1056 ± 10 Ma (1σ, n = 1) (3) metamorphic overgrowths ranging in age between 1017 ± 6 Ma and 992 ± 7 Ma (1σ) corresponding to the regional M1 Sveconorwegian granulite facies metamorphism, and (4) overgrowths corresponding to M2 UHT contact metamorphism giving values of 922 ± 14 Ma (2σ, n = 6). Recrystallized areas in zircon from both areas define a further age group at 974 ± 13 Ma (2σ, n = 4). This study presents the first evidence from Rogaland for new growth of zircon resulting from UHT contact metamorphism. More importantly, it shows the survival of magmatic and regional metamorphic zircon relics in rocks that experienced a thermal overprint of c. 950 °C for at least 1 Myr. Magmatic and different metamorphic zones in the same zircon are sharply bounded and preserve original crystallization age information, a result inconsistent with some experimental data on Pb diffusion in zircon which predict measurable Pb diffusion under such conditions. The implication is that resetting of zircon ages by diffusion during M2 was negligible in these dry granulite facies rocks. Imaging and Th/U–Y systematics indicate that the main processes affecting zircon were dissolution-reprecipitation in a closed system and solid-state recrystallization during and soon after M1.
    Materialart: Digitale Medien
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  • 6
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 22 (2004), S. 0 
    ISSN: 1525-1314
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: The exhumation of eclogite facies granulites (Omp–Plg–Grt–Qtz–Rt) in the Rychleby Mts, eastern Czech Republic, was a localised process initiated by buckling of crustal layers in a thickened orogenic root. Folding and post-buckle flattening was followed by the main stage of exhumation that is characterized by vertical ductile extrusion. This process is documented by structural data, and the vertical ascent of rocks from a depth of c. 70 to c. 35 km is documented by metamorphic petrology. SHRIMP 206Pb/238U and 207Pb/206Pb evaporation zircon ages of 342 ± 5 and 341.4 ± 0.7 Ma date peak metamorphic conditions. The next stage of exhumation was associated with sideways flat thrusting associated with lateral viscous spreading of granulites and surrounding rocks over indenting adjacent continental crust at a depth of c. 35–30 km. This stage was associated with syntectonic intrusion of a granodiorite sill at 345–339 Ma, emplaced at a crustal depth of c. 25 km. The time required for cooling of the sill as well as for heating of the country rocks brackets this event to a maximum of 250 000 years. Therefore, similar ages of crystallization for the granodiorite magma and the peak of eclogite facies metamorphism of the granulite suggest a very short period of exhumation, limited by the analytical errors of the dating methods. Our calculations suggest that the initial exhumation rate during vertical extrusion was 3–15 mm yr−1, followed by an exhumation rate of 24–40 mm yr−1 during further uplift along a magma-lubricated shear zone. The extrusion stage of exhumation was associated with a high cooling rate, which decreased during the stage of lateral spreading.
    Materialart: Digitale Medien
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  • 7
    Digitale Medien
    Digitale Medien
    [s.l.] : Nature Publishing Group
    Nature 243 (1973), S. 29-30 
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] The west coast of Southern Africa is characterized by linear belts of plutonic and volcanic complexes; if these rocks were generated over plumes and the African plate has moved laterally over them they should appear progressively younger in the same direction, from east to west. The hypothesis may ...
    Materialart: Digitale Medien
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  • 8
    ISSN: 1432-0967
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Notizen: Abstract We report single grain U-Pb ion-microprobe as well as conventional bulk size fraction ages for zircons from 3 metasediment samples of the Moldanubian Complex, Bohemian Massif, one of the largest crystalline complexes of the Hercynian foldbelt in Europe. These are complemented by whole-rock Sm-Nd model ages. The metasediments are of upper amphibolite to granulite grade and come from the Bory Massif in Moravia, NW of Brno (sample AA-1) and from the Varied Group (AA-2) and Monotonous Group (AA-3) in the Ceske Budejovice region of SW Bohemia. Ion-microprobe data for detrital zircons yielded 207Pb/ 206Pb ages between ca. 1750 Ma and 2680 Ma and reflect chronologically heterogeneous source terrains. One grain in sample AA-1 of the Bory granulite massif may be as old as 2684±14 Ma, and this constitutes the oldest reported zircon age for the Hercynian belt of central Europe. The single grain data are much less discordant than previously published conventional U-Pb analyses from bulk zircon samples and suggest a significant early Proterozoic crust-formation event between 2 and 2.2 Ga ago. The size fraction data are compatible with the single grain ages and give a fairly precise definition of the Hercynian event between 347 and 367 Ma ago while their upper Concordia intercept ages between ≈1700 and ≈2050 Ma represent the mean of the respective grain populations and are probably geohronologically meaningless. The Nd whole-rock model ages between 1.7 and 3.0 Ga confirm mid-Proterozoic to Archaean source terrains for the dated metasediments.
    Materialart: Digitale Medien
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  • 9
    ISSN: 1432-0967
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Notizen: Abstract The Onega plateau constitutes part of a vast continental flood basalt province in the SE Baltic Shield. It consists of Jatulian-Ludikovian submarine volcanic, volcaniclastic and sedimentary sequences attaining in places 4.5 km in thickness. The parental magmas of the lavas contained ∼10% MgO and were derived from melts generated in the garnet stability field at depths 80–100 km. The Sm-Nd mineral and Pb-Pb whole-rock isochron ages of 1975 ± 24 and 1980 ± 57 Ma for the upper part of the plateau and a SHRIMP U-Pb zircon age of 1976 ± 9 Ma for its lower part imply the formation of the entire sequence within a short time span. These ages coincide with those of picrites in the Pechenga-Imandra belt (the Kola Peninsula) and komatiites and basalts in the Karasjok-Kittilä belt (Norway and Finnmark). Together with lithostratigraphic, chemical and isotope evidence, these ages suggest the derivation of the three provinces from a single large (∼2000 km in diameter) mantle plume. These plume-generated magmas covered ∼600,000 km2 of the Baltic Shield and represent a major contribution of juvenile material to the existing continental crust at 2.0 Ga. The uppermost Onega plateau lavas have high (Nb/Th)N = 1.4–2.4, (Nb/La)N= 1.1–1.3, positive ɛNd(T) of +3.2 and unradiogenic Pb-isotope composition (μ1 = 8.57), comparable with those of modern oceanic plume-derived magmas (oceanic flood basalt and ocean island basalt). These parameters are regarded as source characteristics. The lower sequences have (Nb/Th)N= 0.58–1.2, (Nb/La)N= 0.52–0.88 and ɛNd(T) =−2.6. They have experienced mixing with 10–30% of continental crust and resemble contaminated lavas from other continental flood basalt provinces. The estimated Nb/U ratios of 53 ± 4 in the uncontaminated rocks are similar to those found in the modern mantle (∼47) suggesting that by 2.0 Ga a volume of continental crust similar to the present-day value already existed.
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  • 10
    Digitale Medien
    Digitale Medien
    Springer
    Contributions to mineralogy and petrology 132 (1998), S. 1-20 
    ISSN: 1432-0967
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Notizen: Abstract The Variscan Erzgebirge represents an antiform with a core of gneisses and mica schists, surrounded by a phyllitic mantle. The Gneiss-Eclogite Unit (GEU), in the central part, is a composite tectonometamorphic assemblage characterized by a HP-HT imprint and comprises migmatitic para- and orthogneisses, HT mylonites, HP granulites, eclogites and garnet peridotites. It is tectonically sandwiched between two major units with distinctly lower PT histories. The GEU experienced a characteristic “kinked” retrograde PT path after HP-HT equilibration with: (1) strong near-isothermal decompression at high temperatures; (2) extensive re-equilibration at medium pressures, followed (3) by rapid cooling during continued uplift. We dated zircons (Pb-Pb evaporation) from granitoid orthogneisses and metapelites of the GEU. The orthogneisses contain euhedral, long-prismatic zircons of igneous origin that provided protolith ages between 470 and 524 Ma. Metapelites retain well-preserved granulite-facies mineral assemblages and contain spherical, multifaceted metamorphic zircons that grew near the peak of HP/HT metamorphism. Inclusions of prograde HP phengite (∼15 kbar) and rutile are included in one such zircon. Metamorphic zircons of three samples from different localities yielded identical 207Pb/206Pb ages of 340.5 ± 0.7 Ma, 341.2 ± 0.5 Ma and 341.6 ± 0.5 Ma respectively. Consideration of these zircon ages with published 39Ar/40Ar white mica ages suggests fast cooling and uplift rates in excess of 50 °C/Ma and 4 km/Ma. This is typical for large-scale extensional tectonic unroofing of the ultra-deep part of a fossil, thickened Variscan continental crust (〉60 km) during continuing continental collision and orogenic collapse.
    Materialart: Digitale Medien
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