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dc.contributor.authorMakin, Sean W.
dc.contributor.supervisorChris Clarken_US
dc.contributor.supervisorTim Johnsonen_US
dc.date.accessioned2021-03-23T07:23:18Z
dc.date.available2021-03-23T07:23:18Z
dc.date.issued2021en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/83006
dc.description.abstract

This thesis produced new pressure–temperature–time constraints on the 4D evolution of the southern Western Gneiss Complex (WGC) and overlying rocks, confirming that the Nordfjord–Sogn detachment (NSD) played a key role in developing their present-day positions. This coupled with data from further north lending weight to the WGC exhuming from flat-slab conditions. Recognition of large amounts of mechanical heating surrounding the NSD was key, with potential implications to large-scale crustal structures.

en_US
dc.publisherCurtin Universityen_US
dc.titleA Geochronological and Thermobarometric Investigation of Eclogites and overlying Hyllestad Schists from the Southern Western Gneiss Complex, Norwayen_US
dc.typeThesisen_US
dcterms.educationLevelMResen_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusFulltext not availableen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidMakin, Sean W. [0000-0001-5057-1977]en_US
dc.date.embargoEnd2023-03-23


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