Diffusion of Ti and some Divalent Cations in Olivine as a Function of Temperature, Oxygen Fugacity, Chemical Potentials and Crystal Orientation

Jollands, M. C.; Hermann, Jörg; O’Neill, H. St. C.; Spandler, C.; Padrón-Navarta, J. A. (2016). Diffusion of Ti and some Divalent Cations in Olivine as a Function of Temperature, Oxygen Fugacity, Chemical Potentials and Crystal Orientation. Journal of petrology, 57(10), pp. 1983-2010. Oxford University Press 10.1093/petrology/egw067

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Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences > Petrology
08 Faculty of Science > Institute of Geological Sciences

UniBE Contributor:

Hermann, Jörg

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

0022-3530

Publisher:

Oxford University Press

Language:

English

Submitter:

Jörg Hermann

Date Deposited:

20 Apr 2017 10:03

Last Modified:

20 Apr 2017 10:03

Publisher DOI:

10.1093/petrology/egw067

BORIS DOI:

10.7892/boris.96319

URI:

https://boris.unibe.ch/id/eprint/96319

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