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  • 2010-2014  (854)
  • 2005-2009  (396)
  • 1945-1949  (4)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Hoboken, NJ : Wiley
    Call number: M 08.0418
    Description / Table of Contents: Contents: Part I: Principles of Atomic Physics. 1. Nuclear Systematics. 2. Decay Modes of Radionuclides. 3. Radioactive Decay. 4. Geochronometry. Part II: Radiogenic Isotope Geochronometers. 5. The Rb-Sr Method. 6. TheK-ArMethod. 7. The 40 Ar / 39 Ar Method. 8. TheK-CaMethod. 9. The Sm-Nd Method. 10. The U-Pb, Th-Pb, and Pb-Pb Methods. 11. The Common-Lead Method. 12. The Lu-Hf Method. 13. The Re-Os Method. 14. The La-Ce Method. Part III: Geochemistry of Radiogenic Isotopes. 16. Mixing Theory. 17. Origin of Igneous Rocks. 18. Water and Sediment. 19. The Oceans. Part IV: Short-Lived Radionuclides. 20. Uranium/Thorium-Series Disequilibria. 21. Helium and Tritium. 22. Radiation-Damage Methods. 23. Cosmogenic Radionuclides. 24. Extinct Radionuclides. 25. Thermonuclear Radionuclides. Part V: Fractionation of Stable Isotopes. 26. Hydrogen and Oxygen. 27. Carbon. 28. Nitrogen. 29. Sulfur. 30. Boron and Other Elements. Index. International Geological Timescale (2002).
    Type of Medium: Monograph available for loan
    Pages: XXVII, 897 S. , graph. Darst., Kt. , 25 cm
    Edition: 3rd Ed., [completely updated and expanded]
    ISBN: 0471384372
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Paris : L'Harmattan
    Call number: AWI P5-14-0014 ; AWI P5-14-0013
    Description / Table of Contents: Contents: Preface: The Arctic and the Configuration of the Stars / Alain Faure. - Introduction: The Arctic, Innovative Thinking for a New Region? / Cécile Pelaudeix. - Towards an ice-free Arctic Ocean? / Jérôme Weiss. - Iggiagruk is my Inupiaq name / William l. Iggiagruk Hensley. - Canadian Arctic Security and ClimateChange: Going Beyond a Traditional Security Approach / Heather N. NicolInuit. - Governance in a Changing Environment: a Scientific or a Political Project? / Cécile Pelaudeix. - Indigenous peoples of Russia as political actors / Natalie Novik. - Sustainable Development and the Greening of Sovereignty in the Canadian Arctic / Paule Halley & Marie-Eve Mercier. - Continental Shelves and Maritime Boundaries in the Arctic: the New Cold War Will Not Take Place / Frédéric Lasserre. - Towards a Common Polar NavigationCode: when the Antarctic and the Arctic Converge / Anne Choquet. - Economic activities in the Arctic Ocean: Universal, Regional and National Regulation / Alexander N. Vylegzhanin. - Northern Geopolitics in Flux: From a frontier mentality to peaceful cooperation / Lassi Heininen. - International and Regional Regulation of the Arctic: is there a role for theEuropean Union? / Clive Archer. - Concluding Remarks: The New Mediterranean / Robert Howell Griffiths.
    Description / Table of Contents: The Arctic region is undergoing dramatic transformation. Rapid change due to climate warming is currently affecting the Arctic more than any other region in the world: the permafrost is melting, glaciers are receding, the sea ice is shrinking. With the melting of ice, the circumpolar region is subject to increasing forces of globalization, and navigation through the Northwest and the Northeast passages is rapidly emerging as a practical and commercial proposition. Moreover, the Arctic may be home to 30 per cent of the planet's undiscovered natural gas reserves and 13 per cent of its undiscovered oil. "What holds the Arctic together?" The emphasis here is on convergence, rather than divergence, the Arctic's centrality not its eccentricity. The contributions gathered together in this book all address essential questions posed by geophysicists, political scientists, jurists, geographers and historians. How can science calculate and assess the scale of change in this geographic space, in particular concerning the melting of ice? To what extent are the native populations listened to and act as active participants in decision-making concerning the Arctic? In the context of post-Cold War international and regional cooperation, what is the present state of Arctic governance? How are the Arctic States themselves cooperating in facing the challenges that lie ahead? Are existing juridical arrangements adequate? What role in the Arctic can be played by actors such as the European Union? To what extent are other powerful countries, such as the Asian giants, taking a direct interest in the development of the Arctic?
    Type of Medium: Monograph available for loan
    Pages: 193 S. : Ill., graph. Darst., Kt.
    ISBN: 9782296992191
    Series Statement: Logiques politiques
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 3
    Call number: PIK B 160-09-0179
    Description / Table of Contents: Contents: PART I: INTRODUCTION TO THE BOOK - 1. Introduction ; PART II: GREENHOUSE GAS EMISSIONS TRADING IN THE EU - 2. Legislative Choices and Legal Values: Considerations on the Further Design of the European Greenhouse Gas Emissions Trading Scheme from a Viewpoint of Democratic Accountability ; 3. Too Much Harmonization? An Analysis of the Commission's Proposal to Amend the EU ETS from the Perspective of Legal Principles ; 4. The "Emissions Trading Scheme" Case-Law: Some New Paths for a Better European Environmental Protection ; 5. European Emissions Trading and the Polluter-Pays Principle: Assessing Grandfathering and Over-Allocation ; 6. EU Greenhouse Gas Emissions Trading and Competition Law ; 7. The Underestimated Possibility of Ex Post Adjustments: Some Lessons from the Initial Greenhouse Gas Emissions Trading Scheme ; 8. Economic Impacts of the EU ETS: Preliminary Evidence ; PART III: ALTERNATIVES AND NEW DEVELOPMENTS - 9. Regional Regulatory Initiatives Addressing GHG Leakage in the USA ; 10. Domestic Initiatives in the UK ; 11. Linking the EU ETS to Other Emissions Trading Schemes ; 12. Expansion of the EU ETS: The Case of Emissions Trading for Aviation ; 14. The European Emissions Trading System: Auctions and their Challenges ; PART IV: CONCLUSIONS: FUTURE LOOK - 15. Concluding Remarks ; Index
    Type of Medium: Monograph available for loan
    Pages: XII, 411 S. : graph. Darst.
    ISBN: 9781847208989
    Series Statement: New horizons in environmental law
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 4
  • 5
    Publication Date: 2010-07-01
    Print ISSN: 0921-8181
    Electronic ISSN: 1872-6364
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 6
    Publication Date: 2006-05-01
    Print ISSN: 0886-7798
    Electronic ISSN: 1878-4364
    Topics: Architecture, Civil Engineering, Surveying
    Published by Elsevier
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  • 7
    Publication Date: 2020-02-12
    Description: The southern Hikurangi Subduction Margin is characterized by significant accretion with predicted high rates of fluid expulsion. Bottom simulating reflections (BSRs) are widespread on this margin, predominantly occurring beneath thrust ridges. We present seismic data across the Porangahau Ridge on the outer accretionary wedge. The data show high-amplitude reflections above the regional BSR level. Based on polarity and reflection strength, we interpret these reflections as being caused by free gas. We propose that the presence of gas above the regional level of BSRs indicates local upwarping of the base of gas hydrate stability caused by advective heatflow from upward migrating fluids, although we cannot entirely rule out alternative processes. Simplified modelling of the increase of the thermal gradient associated with fluid flow suggests that funnelling of upward migrating fluids beneath low-permeability slope basins into the Porangahau Ridge would not lead to the pronounced thermal anomaly inferred from upwarping of the base of gas hydrate stability. Focussing of fluid flow is predicted to take place deep in the accretionary wedge and/or the underthrust sediments. Above the high-amplitude reflections, sediment reflectivity is low. A lack of lateral continuity of reflections suggests that reflectivity is lost because of a destruction of sediment layering from deformation rather than gas-hydrate-related amplitude blanking. Structural permeability from fracturing of sediments during deformation may facilitate fluid expulsion on the ridge. A gap in the BSR in the southern part of the study area may be caused by a loss of gas during fluid expulsion. We speculate that gaps in otherwise continuous BSRs that are observed beneath some thrusts on the Hikurangi Margin may be characteristic of other locations experiencing focussed fluid expulsion.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 23 (2005), S. 0 
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The development of shear zones at mid-crustal levels in the Proterozoic Willyama Supergroup was synchronous with widespread fluid flow resulting in albitization and calcsilicate alteration. Monazite dating of shear zone fabrics reveal that they formed at 1582 ± 22 Ma, at the end of the Olarian D3 deformational event and immediately prior to the emplacement of regional S-type granites. Two stages of fluid flow are identified in the area: first an albitizing event which involved the addition of Na and loss of Si, K and Fe; and a second phase of calcsilicate alteration with additions of Ca, Fe, Mg and Si and removal of Na. Fluid fluxes calculated for albitization and calcsilicate alteration were 5.56 × 109 to 1.02 × 1010 mol m−2 and 2.57 × 108–5.20 × 109 mol m−2 respectively. These fluxes are consistent with estimates for fluid flow through mid-crustal shear zones in other terranes. The fluids associated with shearing and alteration are calculated to have δ18O and δD values ranging between +8 and +11‰, and −33 and −42‰, respectively, and ɛNd values between −2.24 and −8.11. Our results indicate that fluids were derived from metamorphic dehydration of the Willyama Supergroup metasediments. Fluid generation occurred during prograde metamorphism of deeper crustal rocks at or near peak pressure conditions. Shear zones acted as conduits for major crustal fluid flow to shallow levels where peak metamorphic conditions had been attained earlier leading to the apparent ‘retrograde’ fluid-flow event. Thus, the peak metamorphism conditions at upper and lower crustal levels were achieved at differing times, prior to regional granite formation, during the same orogenic cycle leading to the formation of retrograde mineral assemblages during shearing.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Berkeley, Calif. : Berkeley Electronic Press (now: De Gruyter)
    Review of law and economics 3.2007, 1, art7 
    ISSN: 1555-5879
    Source: Berkeley Electronic Press Academic Journals
    Topics: Law , Economics
    Notes: This paper provides a coherent framework for classifying cases with multiple tortfeasors in relation to the efficient allocation of liability across the tortfeasors. We construct a simple model in which various tortfeasors contribute to a loss, and consider efficient liability rules under various assumptions.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Terra nova 17 (2005), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: In situ U–Th–Pb geochronology on monazite using Electron Probe Micro Analyser has been performed on migmatite in the southern French Variscan Massif Central in order to decipher its complex history. After the Early Visean (340 Ma) nappe stacking, the Cévennes area experienced a regional migmatization already dated 330–325 Ma in northern Cévennes. In these rocks two monazite populations are recognized on the basis of petrology texture and geochemistry. The oldest monazite generation that appears as inclusion in K-feldspar is dated at 331 ± 4 Ma. This age complies with that of the crustal melting experienced by the Cévennes metamorphic series. The youngest monazite generation is interstitial and gives an age of 320 ± 5 Ma. A hydrothermal origin, coeval with the peraluminous magmatism that predates the formation of the Late Carboniferous Velay Dome is proposed as a working hypothesis to account for the formation of this second monazite generation.
    Type of Medium: Electronic Resource
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