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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
-
Gabon
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Oklo (1)
-
-
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North Africa
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Tunisia (1)
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Southern Africa
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South Africa (1)
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Asia
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Arabian Peninsula
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Saudi Arabia (1)
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Far East
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China
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Ordos Basin (1)
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Qaidam Basin (1)
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Japan
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Honshu
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Gifu Japan (4)
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Tono Japan (3)
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Gobi Desert (1)
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Kemerovo Russian Federation
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Middle East
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Canada
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Ontario
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Western Canada
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British Columbia
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Saskatchewan
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Commonwealth of Independent States
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Russian Federation
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Primary terms
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absolute age (5)
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Africa
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Asia
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Japan
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Canada
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Western Canada
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carbon
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Cenozoic
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Quaternary
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Holocene (1)
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Bandelier Tuff (1)
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Bishop Tuff (1)
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upper Pleistocene (2)
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Tertiary
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Neogene
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Miocene
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Crater Flat Tuff (1)
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Mizunami Group (1)
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Paintbrush Tuff (4)
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Tiva Canyon Member (4)
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Topopah Spring Member (6)
-
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Paleogene
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Eocene (1)
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Tokai Group (1)
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clay mineralogy (16)
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Germany
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hydrology (19)
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igneous rocks
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diabase (1)
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granites (9)
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volcanic rocks
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basalts (2)
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ignimbrite (1)
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tuff (8)
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welded tuff (3)
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rhyolites (1)
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intrusions (1)
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Invertebrata
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Mollusca (1)
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isotopes
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radioactive isotopes
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stable isotopes
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O-18/O-16 (2)
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land subsidence (1)
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Mesozoic
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Cretaceous (5)
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uranium (8)
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alkali metals
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Cs-137 (1)
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alkaline earth metals
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Sr-87/Sr-86 (1)
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Al-27 (1)
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paleoclimatology (1)
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Paleozoic
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Ordovician
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Queenston Shale (1)
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Permian
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Basic Research on Rockburst Control Technology for Deep Well Filling of Municipal Solid Waste
Geophysical characterization of a leachate plume from a former municipal solid waste disposal site: A case study on Norman landfill
Investigating the effective resistivity of reinforced concrete waste storage tanks at the Hanford Site
Natural and Anthropogenic Analogues for High-Level Nuclear Waste Disposal Repositories: A Review
Elastic vertically transversely isotropic full-waveform inversion using cross-gradient constraints — An application toward high-level radioactive waste repository monitoring
Change of crackling noise in granite by thermal damage: Monitoring nuclear waste deposits
Hydrochronology of a proposed deep geological repository for low- and intermediate-level nuclear waste in southern Ontario from U–Pb dating of secondary minerals: response to Alleghanian events
Hydrochronology of a proposed deep geological repository for low- and intermediate-level nuclear waste in southern Ontario from U–Pb dating of secondary minerals: response to Silurian and Cretaceous events
Multiple roles of clays in radioactive waste confinement – introduction
Abstract Geological disposal provides the safe long-term management solution for higher-activity radioactive waste. The development of a repository (or geological disposal facility) requires a systematic and integrated approach, taking into account the characteristics of the waste to be emplaced, the enclosing engineered barriers, and the host rock and its geological setting. Clays and clayey material are important in the development of many national geological disposal systems. Clays exhibit many interesting properties, and are proposed both as host rocks and as material for engineered barriers. Whatever their use, clays present various characteristics that make them high-quality barriers to the migration of radionuclides and chemical contaminants. As host rocks, clays are, in addition, hydrogeologically, geochemically and mechanically stable over geological timescales (i.e. millions of years).
Site screening of clay formations in NW China as host rocks for a high-level radioactive waste disposal repository
Abstract Deep geological disposal of high-level radioactive waste (HLW) in a repository with a system of engineered and natural barriers has been recognized as an appropriate disposal concept by Chinese authorities since 2003, and both crystalline rocks and argillaceous rocks are considered as the candidate host rocks for HLW disposal repository. The 1:200 000 regional survey indicated that there are potential clay formations in Mesozoic–Cenozoic sedimentary basins in NW China. Five candidate areas have been suggested with potential clay formations including the Tamusu and Suhongtu areas with upper K 1 Bayingebi clay formations in the east Bayingebi Basin, in the Inner Mongolia Autonomous Region. On the basis of a detailed ground geological, hydrological and geophysical surveys, two test boreholes drilled to a depth of 800 m in the Tamusu area revealed that there are three lacustrine-facies clay formations (K 1 b 2-3 , K 1 b 2-2 and K 1 b 2-1 ). The thickness of the K 1 b 2-3 and K 1 b 2-2 clay formations is about 300–600 m with sandstone and siltstone interbeds, while the thickness of the K 1 b 2-1 homogeneous clay formation is more than 200 m with the depth of 450 m below the surface. The spatial extension of the clay formations could meet the fundamental criteria to ensure the long-term safety of the repository. Initial mineralogical studies on core samples indicated that the mineral assemblage is dominated by analcite, kaolinite, illite and dolomite. The homogeneous argillaceous rocks rich in analcite in Tamusu area could be a new type of host rock for a HLW disposal repository.
Origin and 87 Rb– 87 Sr age of porewaters in low permeability Ordovician sediments on the eastern flank of the Michigan Basin, Tiverton, Ontario, Canada
Electrical resistivity tomography and distributed temperature sensing monitoring to assess the efficiency of horizontal recirculation drains on retrofit bioreactor landfills
TESTING HIGH-VOLTAGE ELECTRICAL DISCHARGES IN DISINTEGRATING CLAYSTONE FOR ISOTOPIC AND MINERALOGICAL STUDIES: AN EXAMPLE USING OPALINUS CLAYSTONE
The use of Ankara Clay as a compacted clay liner for landfill sites
A case study assessing thermal activity at a significant geotourism locality of Ema coal tailing dumps in the mining landscape of Ostrava, Czech Republic
Abstract It is internationally accepted that the safest and most sustainable option for managing radioactive waste is geological disposal, utilizing both engineering and geology to isolate the waste and contain the radioactivity. This Special Publication contains 25 scientific studies presented at the 6th conference on ‘Clays in natural and engineered barriers for radioactive waste confinement’ held in Brussels, Belgium in 2015. The conference and this resulting volume cover many of the aspects of clay characterization and behaviour considered at various temporal and spatial scales relevant to the confinement of radionuclides in clay, from basic phenomenological process descriptions to the global understanding of performance and safety at repository and geological scales. The papers in this volume consider research into argillaceous media under the following topic areas: large-scale geological characterization; general strategy for clay-based disposal systems; geomechanics; mass transfer; bentonite evolution and gas transfer. The collection of different topics presented in this Special Publication demonstrates the diversity of geological repository research.