dc.contributor.author | Crowley, Peter D. | |
dc.coverage.spatial | NARVIK | |
dc.coverage.spatial | 13312 Frostisen | |
dc.coverage.spatial | HAMARØY | |
dc.date.accessioned | 2020-08-26T09:06:45Z | |
dc.date.available | 2020-08-26T09:06:45Z | |
dc.date.issued | 1989 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674182 | |
dc.description.abstract | The Sitas area contains rock derived from the pre-Caledonian Scandinavian craton and from an accreted Caledonian fore-arc complex. These rocks form the par-authocthonous (?) Rombak Complex which can be tied stratigraphically to Baltica and three allochthons which from the base upwards are: the Storriten Complex, the Langvatn nappe and the Marko nappe. The Storriten Complex is a schuppen-zone composed of rocks derived from hinterland equivalents of the Rombak Complex while the Langvatn and Marko nappes are part of an accreted fore-arc terrane which can be correlated with parts of the Middle Køli Nappe Complex (MNKC). The Marko nappe contains mafic rocks whose geochemical affinites suggest derivation from both MORB-like and arc-like sources. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU Bulletin (416) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | STRUKTURGEOLOGI | |
dc.subject | TEKTONIKK | |
dc.subject | KALEDONSKE FJELLKJEDE | |
dc.subject | KARTLEGGING | |
dc.subject | OMDANNING | |
dc.title | The Tectonostratigraphy and structural evolution of the Sitas Area, North Norway and Sweden (68°N). | |
dc.type | Journal article | |
dc.description.localcode | 35213 | |
dc.source.pagenumber | 25-46 | |