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dc.contributor.authorHannah, J.
dc.contributor.authorStein, H.
dc.contributor.authorWieser, M.
dc.contributor.authorDe Laeter, John
dc.contributor.authorVarner, M.
dc.date.accessioned2017-01-30T12:14:46Z
dc.date.available2017-01-30T12:14:46Z
dc.date.created2009-03-05T00:57:10Z
dc.date.issued2007
dc.identifier.citationHannah, J. and Stein, H. and Wieser, Michael and De Laeter, John and Varner, M. 2007. Molybdenum isotope variations in molybdenite: vapor transport and Rayleigh fractionation of Mo. Geology. 35 (8): pp. 703-706.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/19617
dc.identifier.doi10.1130/G23538A.1
dc.description.abstract

Molybdenum isotopes in 20 molybdenite samples, dated by the Re-Os method and representing a range of geologic settings, show mass-dependent fractionation spanning 0.63 per atomic mass unit (amu). Previous Mo isotope data for molybdenite reveal variations in fractionation of <0.5/amu. Interpretation of these data is hampered, however, by limited sample numbers in each study, lack of a common standard for interlaboratory comparison, and limited range of geologic settings. Here we show that Mo isotope compositions of molybdenites do not correlate with crystallization temperature, age, geographic distribution, or geologic conditions. Rather, Rayleigh distillation may explain variations of as much as 0.34/amu in a single molybdenite occurrence, exceeding the proposed variability in average continental crust. Vapor transport and rapid precipitation of Mo in propagating fractures may account for isotope fractionation of Mo (and perhaps other metals) at very small scales. If so, the average isotopic composition of Mo at each molybdenite occurrence may be representative of bulk crust. Our results suggest that the isotopic composition of Mo delivered to the oceans is uniform geographically and through geologic time.

dc.publisherGeological Society of America
dc.titleMolybdenum isotope variations in molybdenite: vapor transport and Rayleigh fractionation of Mo
dc.typeJournal Article
dcterms.source.volume35
dcterms.source.startPage703
dcterms.source.endPage706
dcterms.source.issn00917613
dcterms.source.titleGeology
curtin.note

Publisher's address is: Geological Society of America, P.O. Box 9140, Boulder, CO 80301-9140 USA (http://www.geosociety.org).

curtin.note

Copyright © 2007 Geological Society of America

curtin.departmentDepartment of Imaging and Applied Physics
curtin.accessStatusFulltext not available
curtin.facultyDepartment of Medical Imaging and Applied Physics
curtin.facultySchool of Science
curtin.facultyFaculty of Science and Engineering


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