Structure of the upper mantle below soouth-central Saskatchewan from teleseismic travel-time inversion
An array of three-component seismographs was deployed over the central Trans-Hudson Orogen from October 1994 to July 1996 with the objective of characterizing subcrustal lithospheric structure below an area with diamondiferous kimberlite occurance. The twodimensional array consisted of nine broad...
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| Format: | Others |
| Language: | English |
| Published: |
2009
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| Online Access: | http://hdl.handle.net/2429/5762 |
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