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  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 02.0137
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: viii, 288 S.
    ISBN: 1862390932
    Series Statement: Geological Society special publication 190
    Classification:
    A. 3.9.
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Description / Table of Contents: The age of the Earth has long been a subject of great interest to scientists from many disciplines, particularly geologists, biologists, physicists and astronomers. This volume, The Age of the Earth: from 4004 BC to AD 2002, brings together contributors from these different subjects, along with historians, to produce a comprehensive review of how the Earth’s age has been perceived since ancient times. Touching on the works of eminent scholars from the seventeenth to nineteenth centuries, it describes how concepts of the Earth’s history changed as geology slowly separated itself from religious orthodoxy to emerge as a rigorous and self-contained science. Fossils soon became established as useful markers of relative age, while deductions made from geomorphological processes enabled the discussion of time in terms of years. By the end of the nineteenth century biologists and geologists were fiercely debating the issue with physicists who were unwilling to give them the time needed for evolution or uniformitarianism. With the discovery of radioactivity, attempts to calculate the Earth’s age entered a new era, although these early pioneers in radiometric dating encountered many difficulties, both technical and intellectual, before the enormity of geological time was fully recognized. This effort affected both the theory and practice of geology. Geochronology was largely responsible for it maturing into a professional scientific discipline, as increasingly refined techniques measured not only the age of the rocks, but the rate of processes which now elucidate many aspects of the Earth’s evolution. Even today the Earth’s chronology remains a contentious topic - particularly for those dating the oldest rocks - and it is implicated in debates surrounding our hominid ancestors, the origins and development of life, and the age of the universe. The Age of the Earth: from 4004 bc to AD 2002 will be of particular interest to geologists, geochemists, and historians of science, as well as astronomers, archaeologists, biologists and the general reader with an interest in science.
    Pages: Online-Ressource (VI, 288 Seiten)
    ISBN: 1862390932
    Language: English
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  • 3
    Publication Date: 1993-03-01
    Description: The results of a reconnaissance apatite fission track study from southeast Ireland are compared with modelled ages and length distributions predicted using both traditional thermal histories and the thermal history indicated by the fission track age and length data. All samples have experienced total annealing during the Variscan orogeny. There is strong evidence for significant post-Variscan, pre-Mid Jurassic heating and cooling. The modelling also recognizes a third thermal event subsequent to 100 Ma. The implications of these results are examined in terms of the timing and extent of subsidence and inversion along the northern margin of the North Celtic Sea Basin.
    Print ISSN: 0016-7568
    Electronic ISSN: 1469-5081
    Topics: Geosciences
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  • 4
    Publication Date: 1993-01-01
    Description: Elevated palaeotemperatures prior to Early Tertiary cooling, which affected wide areas of the UK region, have been revealed by Apatite Fission Track Analysis (AFTA™). All available evidence suggests that palaeogeothermal gradients were close to present values and that much of the observed heating was due to greater depth of burial, by 1 to 2 km or more of section that was subsequently removed by uplift and erosion. Uplift and erosion were not restricted to local inversion axes. The palaeotemperature data suggest a broad, regional warping, producing kilometre-scale Tertiary uplift and erosion across a wide area, within which recognized inversion axes represent local regions of maximum uplift and erosion. AFTA data show no thermal effects associated with Cimmerian unconformities, and any heating associated with Cimmerian events was of lesser magnitude than Late Cretaceous to Early Tertiary heating. Over much of the UK region, source rocks attained maximum temperatures and reached peak maturity during this later heating episode. The regional extent of heating at this time and its significance to hydrocarbon source rock maturation have not been fully recognized in the past. The timing of the events described here suggests a link to the development of the Atlantic margin, Laramidé inversion tectonics and the onset of Alpine tectonism. However, definitive answers to such questions must await further research, particularly involving integration of AFTA and other thermal indicators with structural and geophysical data
    Electronic ISSN: 2047-9921
    Topics: Geosciences
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