Geophysical studies of saline fluids in the deep crust
Geophysical studies have shown that the lower continental crust, especially in Phanerozoic areas, is commonly more conductive and reflective and has a lower seismic velocity than what is expected from the composition of xenoliths and exposed lower crustal terrains. These anomalous in situ properties...
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| Format: | Others |
| Language: | English en |
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2018
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| Online Access: | https://dspace.library.uvic.ca//handle/1828/9586 |