Disequilibrium textures in the Centre Hill complex, Munro Township, Ontario.
The Centre Hill complex is part of the mafic to ultramafic Munro Lake sill that occurs within the Stoughton-Roquemaure Group of the Abitibi Subprovince. The complex is approximately 450 m thick and consists of alternating layers of peridotite and clinopyroxenite overlain by 250 m of gabbroic rocks....
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/7614 http://dx.doi.org/10.20381/ruor-6875 |