Magnetic subfabrics of the Whistle Offset dyke and embayment, Sudbury Impact Structure, Sudbury, Ontario
Quartz-diorite Offset dykes from the 1850 Ma Sudbury Impact Structure stem from the Sudbury Igneous Complex (SIC) and extend into the footwall rocks in radial and concentric patterns with respect to the SIC. The dykes formed by emplacement of magma derived from the impact melt body into radial and c...
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| Format: | Others |
| Language: | en |
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University of Ottawa (Canada)
2013
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| Online Access: | http://hdl.handle.net/10393/26913 http://dx.doi.org/10.20381/ruor-11826 |