| dc.date.accessioned | 2018-09-25T07:23:21Z | |
| dc.date.available | 2018-09-25T07:23:21Z | |
| dc.date.issued | 2018 | |
| dc.identifier.uri | http://hdl.handle.net/10852/64930 | |
| dc.description.abstract | Volcanoes are both threat to life and source of economic wealth, however little is known about the processes in the Earth’s crust leading to their origin. Laboratory models are used to shed light on the otherwise inaccessible interactions of hot, molten rock (magma) and its surrounding rocks in the underground. In the future, the knowledge gained from using these models may help forecasting potential risks and improve exploration for resources and geothermal energy.
Vulkaner er en trussel mot livet på jorda og en kilde til økonomisk rikdom, likevel er lite kjent om prosessene i jordskorpen som fører til deres opprinnelse. Laboratoriemodeller brukes til å kaste lys over det ellers utilgjengelige samspillet mellom varm, smeltet stein (magma) og de omkringliggende bergartene i under-grunnen. I fremtiden kan kunnskapen fra disse modellene bidra til å forutse po-tensielle farer og forbedre leting etter ressurser og geotermisk energi. | en_US |
| dc.language.iso | en | en_US |
| dc.relation.haspart | Paper I: Schmiedel, T., Kjoberg, S., Planke, S., Magee, C., Galland, O., Schofield, N., Jackson, C.A.-L., Jerram, D.A., (2017). Mechanisms of overburden deformation associated with the emplacement of the Tulipan sill, mid-Norwegian margin. Interpretation 5, SK23-SK38. DOI: 10.1190/int-2016-0155.1 The article is included in the thesis. Also available at http://urn.nb.no/URN:NBN:no-63809 | |
| dc.relation.haspart | Paper II: Kjoberg, S., Schmiedel, T., Planke, S., Svensen, H.H., Millett, J.M., Jerram, D.A., Galland, O., Lecomte, I., Schofield, N., Haug, Ø.T., Helsem, A., (2017). 3D structure and formation of hydrothermal vent complexes at the Paleocene-Eocene transition, the Møre Basin, mid-Norwegian margin. Interpretation 5, SK65-SK81. DOI: 10.1190/int-2016-0159.1 The article is included in the thesis. Also available at http://urn.nb.no/URN:NBN:no-63693 | |
| dc.relation.haspart | Paper III: Schmiedel, T., Galland, O., Breitkreuz, C., (2017). Dynamics of sill and laccolith emplacement in the brittle crust: role of host rock strength and deformation mode. Journal of Geophysical Research: Solid Earth 122, 8860–8871. DOI: 10.1002/2017JB014468 The article is included in the thesis. Also available at http://urn.nb.no/URN:NBN:no-63818 | |
| dc.relation.haspart | Paper IV: Schmiedel, T., Galland, O., Haug, Ø.T., Dumazer, G., Breitkreuz, C., (submitted). Coulomb failure of Earth's brittle crust controls growth, emplacement and shapes of igneous sills, saucer-shaped sills and laccoliths. To be published. The paper is not available in DUO awaiting publishing. | |
| dc.relation.uri | http://urn.nb.no/URN:NBN:no-63809 | |
| dc.relation.uri | http://urn.nb.no/URN:NBN:no-63693 | |
| dc.relation.uri | http://urn.nb.no/URN:NBN:no-63818 | |
| dc.title | Dynamics of sub-volcanic systems in sedimentary basins and related mechanisms of host rock deformation | en_US |
| dc.type | Doctoral thesis | en_US |
| dc.creator.author | Schmiedel, Tobias | |
| dc.identifier.urn | URN:NBN:no-67464 | |
| dc.type.document | Doktoravhandling | en_US |
| dc.identifier.fulltext | Fulltext https://www.duo.uio.no/bitstream/handle/10852/64930/1/Schmiedel-PhD-2018.pdf | |