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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Vredefort Dome (South Africa). ; Electronic books.
    Description / Table of Contents: Examining the astrology, historical context and life science of the Vredefort crater, this volume presents a rare view into the early stages of planet Earth. The geological, archaeological and cultural heritage of the region is also discussed in this overview.
    Type of Medium: Online Resource
    Pages: 1 online resource (337 pages)
    Edition: 3rd ed.
    ISBN: 9783642104640
    Series Statement: Geoparks of the World Series ; v.1
    DDC: 551.397096852
    Language: English
    Note: Intro -- Contents -- Foreword -- Part I -- Chapter 1: The early history of Earth -- Introduction -- Geological change -- Man on the Moon -- Back to the beginning -- Impact -- The oldest rocks -- Time to cool -- Old crust in the Vredefort Dome -- Rifting, oceans, volcanism -- Mountains, fire and ice -- The unique Bushveld magmatic event -- Chapter 2: Chaos and catastrophe -- Introduction -- Extinction or survival -- Meteorite-impact catastrophes -- Normal (background) versus mass extinctions -- The Smoking gun! -- Vredefort -- A brief look at the impact record in the Solar System -- How did impact science getstarted? -- Craters on the Moon -- From the Moon to the Earth-Moon system -- The impact record on Earth -- The wealth within -- What are the projectiles capable of causing an impact catastrophe? -- Meteors and meteorites -- Large asteroids and comets -- What is an impact crater? -- How can we identify impact structures? -- Shock metamorphism -- Chapter 3: The impact heritage of southern Africa -- Tswaing meteorite crater -- Solving the riddle of the origin of Tswaing -- The search for the meteoritic projectile -- What do we know about the landscape in the Tswaing area prior to the impact? -- What would the catastrophe have been like? -- Were there any witnesses of the catastrophic impact at Tswaing? -- Does Tswaing have a twin? -- South Africa's other giant impact -- Our southern African neighbours -- Testimony of earlier impact catastrophes -- Traces of catastrophe in the Karoo? -- Chapter 4: Vredefort: the largest and oldest impact structure in the World -- The Vredefort Structure revealed -- Getting to know the giant -- Traversing the outer parts of the Vredefort Dome -- The Geology of the Vredefort Dome -- The unique rock formations and deformation in the Vredefort Dome -- The findings of the early Vredefort gealogists -- The second phase. , Craters and breccias -- Shock meta morphism -- The vredefort structure in the 1970s and 1980s -- What do dead elephants in Leningrad have to do with the Vredefort Structure? -- The third phase -- Shocked zircon and a precise agefor the impact event -- How big is 'big'? -- Vredefort research in the 21st century -- Vredefort -- Chapter 5: The recent history of the Vredefort Dome area -- Section 1: Travelling through time -- Introduction -- Stone Age Vredefort Dome -- The Iron Age -- Archaeological research on the Askoppies Late Iron Age site -- Archaeology of the historical period on the dome -- Section 2: Beyond the frontier history of the Vredefort Dome area -- The geographic setting -- Development of towns -- Treading on territorial toes -- Mineral resources -- The Second Anglo-Boer War (1899-1902) -- After the war -- 20th Century developmentand growth -- Development of infrastructure -- Development of tourism -- Workers and forced removals -- Section 3: Flora and fauna of the Vredefort dome -- The Vredefort Dome plants (flora) in a geographical context -- The composition of the flora -- Which biome occurs on the VredefortDome? -- Veld types on the Vredefort Dome -- Factors that affect the vegetation -- The habitats on the Vredefort Dome -- The effect of geology on the vegetation of the Vredefort Dome -- Recent changes in habitats on the Vredefort Dome -- Woody vegetation in the Vredefort Dome -- Fauna in the Vredefort Dome -- Chapter 6: Frequently asked questions -- Frequently asked questions about the Vredefort impact event -- Where is the projectile responsible for the Vredefort impact? -- Do we know from which direction the Vredefort bolide came? -- Do we know how large the bolide was that caused the Vredefort catastrophe? -- Could any life forms have perished in this catastrophe?. , Would this impact have influenced further development of life? -- Can there be other impact structures of the size of Vredefort, not yet discovered on Earth? -- Major diamond, gold and platinum resources lie close to the Vredefort Dome. Why have no major ore deposits been found in the dome itself? -- Is Vredefort truly unique? -- Is the Cradle of Humankind related to the impact structure? -- Chapter 7: What does the future hold for humankind? -- What does the future hold for humankind? -- Chapter 8: Tourism in the Vredefort Dome -- Outlook -- The International Significance of the Vredefort Dome -- Part II -- Tour guide through the Vredefort Dome -- Stops 1-9: the core of the vredefort dome -- Stop 1: Vredefort Dome World Heritage Site Visitor Centre -- Stop 2: Inlandsee pan and the centre of the Vredefort impact structure -- Stop 3: Ancient oceanic crust at Greenlands -- Stop 4: Broodkop shear zone and bentonite mines -- Stop 5: Steynskraal pelitic granulites - a thermal record -- Stop 6: Pseudotachylitic breccia and gneisses, Parys -- Stop 7: Pseudotachylitic breccia and gneisses in the outer core -- Stop 8: Vredefort Granophyre and Bushman petroglyphs, Daskop -- Stop 9: Vredefort Granophyre and Dominion Group lavas, Iniekom -- Stops 10-22: The collar rocks of the vredefprt dome -- Stop 10: Rocks and metamorphism of the Central Rand Group (Witwatersrand Supergroup), Donkervliet valley -- Stop 11: Vaal River view site and alkali granite -- Stop 12: Gold mining in the Venterskroon area -- Stop 13: Shatter cones in the Booysens Formation, Rooderand -- Stop 14: Amazon gold reef, Rooderand -- Stop 15: Ventersdorp lavas, Askoppies Iron Age settlement and Anglo-Boer War sites on Tygerfontein farm -- Stop 16: Stromatolites and cave in Transvaal rocks of the western collar -- Stop 17: Schoemansdrift Bridge shatter cones. , Stop 18: Dwarsberg (Steenkampsberg) view site -- Stop 19: Rocks and metamorphism of the lower Witwatersrand Supergroup, Kommandonek Nature Reserve -- Stop 20: Impact-induced fold and view site, Parson's Rus -- Stop 21: Coesite-stishovite-bearing quartzite, Kromellenboog Stream -- Stop 22: Witwatersrand Supergroup quartzite, impact fault and Bobbejaanrant viewpoint, Smilin' Thru Resort -- Acknowledgements -- Bibliography -- Glossary -- Appendices -- Appendix 1 -- Appendix 2 -- Appendix 3 -- Index.
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  • 2
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Cryptoexplosion structures--Chesapeake Bay (Md. and Va.). ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (528 pages)
    Edition: 1st ed.
    ISBN: 9783642189005
    Series Statement: Impact Studies
    Language: English
    Note: Impact Studies -- The Chesapeake Bay Crater -- Copyright -- Preface -- Acknowledgments -- Contents -- 1 Introduction -- 2 Geological Framework of Impact Site -- 3 Geophysical Framework of Impact Site -- 4 The Primary Crater -- 5 Secondary Craters -- 6 Synimpact Crater-Fill Deposits -- 7 Initial Postimpact Deposits -- 8 Age of Chesapeake Bay Impact Crater -- 9 Geological Consequences of Chesapeake Bay Impact -- 10 Comparisons with Other Impact Craters -- 11 Comparisons Between lmpactites -- 12 Implications for Impact Models -- 13 Biospheric Effects of Chesapeake Bay Impact -- 14 Residual Effects of Chesapeake Bay Impact -- 15 Summary and Conclusions -- Appendix -- References -- Index.
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  • 3
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: In a recent article in Terra Nova, Kristan-Tollmann and Tollmann (1994) suggested that the Biblical Flood can be explained by seven fragments of a comet that impacted the ocean at seven locations on Earth at 03.00h (C.E.T.) on 23 September, 9545 yr BP. We demonstrate that all the ‘geological proofs’ that allegedly support their conclusions are not supported by the available data on impact cratering. Their hypothesis is based on insufficient and ambiguous data, selective citation, and incomplete comprehension of previous research.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 137 (1999), S. 133-146 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Precambrian Dullstroom Formation of South Africa, which is predominantly composed of basaltic andesites interbedded with subordinate sedimentary and felsic volcanic strata, represents the first phase of an extended period of magmatism that was responsible for the Bushveld Magmatic Province, including the extrusive Rooiberg Group and the intrusive Bushveld Complex. New geochemical and isotopic data for the Dullstroom Formation are presented in an effort to elucidate the petrogenetic processes operative during the initiation of this magmatic episode. The volcanic units of the central portion of the Dullstroom Formation have been subdivided into at least three interbedded compositional groups: low Ti mafic to intermediate units, high-Ti mafic to intermediate units, and high Mg felsic units. High Ti and low Ti volcanic units are similar in some compositional characteristics to basalts of the nearby northern and southern provinces, respectively, of the Mesozoic Karoo continental flood basalts. Isotopic and compositional data for low Ti Dullstroom strata are consistent with bulk assimilation into a melt similar in composition to a southern Karoo basalt of 20% upper continental crust accompanied by 20% fractional crystallization of pyroxene and plagioclase. Isotopic and compositional data for high Ti Dullstroom strata are consistent with magma mixing of 30% northern Karoo K-rich basalt and 70% southern Karoo basalt followed by 20% assimilation of upper continental crust and 20% fractional crystallization of pyroxene and plagioclase. Compositions of high Mg felsic volcanic strata are consistent with 25% assimilation of a mixture of silica-rich sedimentary rock and upper continental crust into a melt similar in composition to low Ti volcanic units with 25% fractional crystallization of pyroxene and plagioclase. However, it has been suggested that compositions of these high Mg felsic strata may also be consistent with interaction of a crustal melt. Assimilation, fractional crystallization, and magma mixing that apparently affected these Dullstroom Formation volcanic strata may have occurred in a series of shallow magma chambers. These data are consistent with the suggestion that Dullstroom Formation volcanic rocks are the result of a mantle plume. Mantle plume origin also is suggested by the large volume of intrusive and extrusive strata associated with this magmatic episode. These data do not support the hypothesis that the Bushveld Complex and the Rooiberg Group formed by impacts of a cluster of comets or asteroids.
    Type of Medium: Electronic Resource
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