Item talk:Q245432
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Geologic isolation of nuclear waste at high latitudes: the role of ice sheets", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70042851", "url": "https://pubs.usgs.gov/publication/70042851" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70042851 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1111/j.1468-8123.2011.00358.x", "url": "https://doi.org/10.1111/j.1468-8123.2011.00358.x" } ], "journal": { "@type": "Periodical", "name": "Geofluids", "volumeNumber": "12", "issueNumber": "1" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Geofluids" } ], "datePublished": "2012", "dateModified": "2013-02-26", "abstract": "Geologic isolation of high-level nuclear waste from the biosphere requires special consideration in countries at high latitudes (>40\u00b0N) owing to the possibility of future episodes of continental glaciation (Talbot 1999). It is now widely recognized that Pleistocene continental glaciations have had a profound effect on rates of sediment erosion (Cuffey & Paterson 2010) and deformation including tectonic thrusting (Pedersen 2005) as well as groundwater flow (Person et al. 2007; Lemieux et al. 2008a,b,c). In addition, glacial mechanical loads may have generated anomalous, or fossil, pore pressures within certain clay-rich confining units (e.g. Vinard et al. 2001). 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