dc.contributor.author | Ekström Tormos, Felix | |
dc.date.accessioned | 2021-07-05T11:35:11Z | |
dc.date.available | 2021-07-05T11:35:11Z | |
dc.date.issued | 2021-07-05 | |
dc.identifier.uri | http://hdl.handle.net/2077/69076 | |
dc.description.abstract | Billdal in southwestern Sweden, is an area dominated by two main rock types, Askim
granite and gabbro. Their density difference makes gravity survey an ideal method to
help map the location of gabbro bodies which are not close to the surface. With the use
of Modelvision, it will also be possible to estimate their volume and get an image of the
gabbro plutons in the area. The gravity anomaly results go from a minimum of -1.83 mgal
in the northern part to a maximum of 5.77 mgal, located in the central area of Lindås.
Several different gabbro models are proposed to explain this extreme gravitaty anomaly. | sv |
dc.language.iso | eng | sv |
dc.relation.ispartofseries | B | sv |
dc.relation.ispartofseries | 1126 | sv |
dc.subject | Gravity anomaly | sv |
dc.subject | gabbro | sv |
dc.subject | Askim granite | sv |
dc.subject | modelling | sv |
dc.subject | ModelVision | sv |
dc.title | Gravity Survey of Mafic Rocks at Billdal | sv |
dc.contributor.department | University of Gothenburg/Department of Earth Sciences | eng |
dc.contributor.department | Göteborgs universitet/Institutionen för geovetenskaper | swe |