The geology, geochemistry and structure of the Mooshla intrusion, Bousquet Mining Centre, Quebec.
The Mooshla intrusion is an elliptical body, 4.0 x 1.5 km and is hosted by the Blake River Group, a fault bounded sequence of bi-modal volcanic and volcaniclastic rocks. The intrusion is calc-alkaline in affinity and comprises four distinct units; (1) cumulate gabbros, (2) quartz diorites, (3) tonal...
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| Format: | Others |
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/7829 http://dx.doi.org/10.20381/ruor-15524 |