Formation of chromitites by assimilation of crustal pyroxenites and gabbros into peridotitic intrusions: North Arm Mountain massif, Bay of Islands ophiolite, Newfoundland, Canada

Author:

Bédard Jean H.,Hébert Réjean

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference92 articles.

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2. Internally consistent solution models for Fe-Mg-Mn-Ti oxides- Fe-Mg-Ti oxides and olivine;Andersen;Am. Mineral.,1991

3. An empirical model for the calculation of spinel-melt equilibria in mafic igneous systems at atmospheric pressure, 1, Chromian spinels;Ariskin;Contrib. Mineral. Petrol.,1996

4. A complex corona between olivine and plagioclase from the Jotun Nappe, Norway, and the diffusion modelling of multimineralic layers;Ashworth;Mineral. Mag.,1992

5. Chromite deposits in the southern Oman ophiolite: Mineralogical constraints;Augé;Miner. Deposita,1987

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