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Mass dependent isotopic fractionation of molybdenum in the solar system

Abstract:

Mass dependent isotope fractionation of stable isotopes between meteorites and planetary materials has been used to assess processes that occurred during formation of Earth and its core. However, thus far little is known about the mass dependent isotope fractionation of Mo in the solar system, and at high temperatures in the Earth, in particular during mantle processes. Molybdenum is a refractory and moderately siderophile element. The processes that might have fractionated Mo in the early...

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Oxford college:
St Hugh's College
Role:
Author

Contributors

Division:
MPLS
Department:
Earth Sciences
Role:
Supervisor
Division:
MPLS
Department:
Earth Sciences
Role:
Supervisor
Publication date:
2013
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
Oxford University, UK
Language:
English
Keywords:
Subjects:
UUID:
uuid:4ad9f7d2-d622-4e62-a188-690d0bb539d6
Local pid:
ora:8872
Deposit date:
2014-08-08

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