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Helium Isotope Dating of Pore Water in the St. Clair Basin

dc.contributor.advisorClarke, W. B.
dc.contributor.authorHatch, David
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-05-05T15:17:03Z
dc.date.available2016-05-05T15:17:03Z
dc.date.issued1984-04
dc.description.abstract<p> An age of approximately 55K years was found for the St. Clair basin clays using helium isotope dating. This is about 5 times larger than the date obtained from the more accepted carbon-14 method and from other geological evidence. Diffusion of helium from crustal rocks against a flow of approximately 0.03-0.05 cm a· ' is the primary reason for this discrepancy. Mixing of the groundwater with a meteoric component has an opposite effect tending to lower the helium age. </p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19225
dc.language.isoenen_US
dc.subjectheliumen_US
dc.subjectisotope datingen_US
dc.subjectpore wateren_US
dc.subjectSt. Clair Basinen_US
dc.titleHelium Isotope Dating of Pore Water in the St. Clair Basinen_US

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