This MSc thesis reprocessed seismic data collected at a site near the Gota River in 2011, focusing on two lines. The two seismic lines ran through a landslide scar zone for a total length of 1 km, both of which used dynamite as the seismic source. The thesis used a standard seismic processing tool for this purpose, with the main processes including static corrections, bandpass filtering, velocity analysis, NMO corrections, stack, and migration. Analysis of the resulting images reveals a coarse-grained layer near the surface, which is in contact with the quick clays overlying them. Bedrock is close to the surface at high elevations and reaches a depth of 90 m under the landslide scar. The reflections are discontinuous at some locations. The first breaks were inverted using tomography methods and the resulting inversion models was correlated with the reflection images. Analysis of the subsurface topography suggests a situation where the quick-clay landslide hazard may be present, the specifics of which need to be combined with other geological and geotechnical investigations and scenario buildings. The high-resolution reflection seismic imaging method has a great promise for quick-clay landslide studies.
| Identifer | oai:union.ndltd.org:UPSALLA1/oai:DiVA.org:uu-479118 |
| Date | January 2022 |
| Creators | Mu, Zhaochen |
| Publisher | Uppsala universitet, Geofysik |
| Source Sets | DiVA Archive at Upsalla University |
| Language | English |
| Detected Language | English |
| Type | Student thesis, info:eu-repo/semantics/bachelorThesis, text |
| Format | application/pdf |
| Rights | info:eu-repo/semantics/openAccess |
| Relation | Examensarbete vid Institutionen för geovetenskaper, 1650-6553 ; 551 |
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