Formation of podiform chromitites by melt/rock interaction in the upper mantle
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics,Economic Geology
Link
http://link.springer.com/content/pdf/10.1007/BF03326400.pdf
Reference22 articles.
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2. Bacuta, G.C., Kay, R.W., Gibbs, A.K., Bruce, R.L. (1990) Platinum-group element abundances and distribution in chromite deposits of the Acoje Block, Zambales ophiolite complex, Philippines. J. Geochem. Explor. 37:113–145
3. Bai, W.-J., Zhou, M.-F., Robinson, P.T. (1993) Possibly diamond-bearing mantle peridotites and podiform chromitites in the Luobusa and Donqiao ophiolites, Tibet. Can. J. Earth Sci. 30: 1650–1659
4. Barnes, S.J., Naldrett, A.J., Gorton, M.P. (1985) The origin of the fractionation of platinum-group elements in terrestrial magmas. Chem. Geol. 53:303–323
5. Campbell, I.H., Murck, B.W. (1993) Petrology of the G and H chromitite zones in the Mountain View Area of the Stillwater complex, Montana. J. Petrol. 34:291–316
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