Cosmic ray muon production of isotopic anomalies in the Earth's crust

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dc.contributor.advisorClayton, Donald W.en_US
dc.creatorMorgan, John Adrianen_US
dc.date.accessioned2018-12-18T21:17:26Zen_US
dc.date.available2018-12-18T21:17:26Zen_US
dc.date.issued1977en_US
dc.description.abstractThe recent discovery of naturally occurring radioactive niobium isotopes, of atomic weight 92 and 94, in commercially prepared niobium admits an explanation in terms of production by the capture of cosmic ray muons by terrestrial molybdenum, and encourages the examination of (u-,xn) mechanisms for their possible role in the origin of other trace isotopic effects.en_US
dc.format.digitalOriginreformatted digitalen_US
dc.format.extent107 ppen_US
dc.identifier.callnoThesis Sp. Sci. 1977 Morganen_US
dc.identifier.citationMorgan, John Adrian. "Cosmic ray muon production of isotopic anomalies in the Earth's crust." (1977) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/104102">https://hdl.handle.net/1911/104102</a>.en_US
dc.identifier.digitalRICE1729en_US
dc.identifier.urihttps://hdl.handle.net/1911/104102en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.titleCosmic ray muon production of isotopic anomalies in the Earth's crusten_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentSpace Scienceen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Scienceen_US
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