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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Postglacial rebound and total water storage variations in the Nelson River drainage basin: a gravity GPS Study, Geological Survey of Canada Open File, 7317</title>
<creator>Lambert, A.</creator>
<creator>Henton, J.</creator>
<creator>MAZZOTTI, Stephane</creator>
<creator>James, T. S.</creator>
<creator>Courtier, N.</creator>
<creator>Huang, J.</creator>
<creator>Van Der Kamp, G.</creator>
<contributor>Risques ; Geological Survey of Canada, Sidney ; Université du Québec - Université du Québec</contributor>
<contributor>Geodetic Survey Division, Sidney ; Université du Québec</contributor>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Geological Survey of Canada, Sidney ; Université du Québec</contributor>
<description>Report</description>
<identifier>hal-00856668</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00856668</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00856668</source>
<source>GM:13-061. Report. 2013, 21 pp. 〈10.4095/292189〉</source>
<identifier>DOI : 10.4095/292189</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.4095/292189</relation>
<language>en</language>
<subject lang=en>hydrogeology</subject>
<subject lang=en>drainage systems</subject>
<subject lang=en>Winnipeg River basin</subject>
<subject lang=en>geographic information system applications</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/other</type>
<type>Other publications</type>
<description lang=en>GPS, absolute gravity and GRACE satellite data have been combined to map postglacial rebound (glacial isostatic adjustment) and to identify large spatial-scale water storage variations in the Nelson River drainage basin. GPS data from 27 continuous sites over the period 1996-2010 with an average time-series length of 10.6 years were combined with data from over 50 regularlysurveyed monuments over the period 1995-2011 to produce an updated vertical velocity map for the basin.</description>
<date>2013-01-14</date>
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