Induced Seismicity in the Dannemora Mine, Sweden
Induced seismicity is a common phenomenon that occurs as soon as the stress state in the subsurface is externally altered in a way that faults are destabilized. It is especially problematic in stable tectonic regions where the area is not used to earthquakes; the infrastructure is not built to withs...
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| Format: | Others |
| Language: | English |
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Uppsala universitet, Geofysik
2015
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| Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-267361 |