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Age constraints on the late Caledonian (Scandian) deformation in the Major Bergen Arc, SW Norway

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dc.contributor.authorFossen, H
dc.contributor.authorDunlap, William James
dc.date.accessioned2015-12-07T22:32:58Z
dc.date.issued2006
dc.date.updated2015-12-07T10:25:56Z
dc.description.abstractThe Ulven Syncline in the Bergen Arcs contains some of the youngest rocks involved in Caledonian orogenic deformation in West Norway. The pelitic Vaktdal Formation contains a Middle Llandovery (439-436 Ma) fauna, providing a maximum age of deposition and
dc.identifier.issn0029-196X
dc.identifier.urihttp://hdl.handle.net/1885/23051
dc.publisherGeological Society Norway
dc.sourceNorsk Geologisk Tidskrift - Norwegian Journal of Geology
dc.subjectKeywords: argon-argon dating; biotite; Caledonian orogeny; deformation; deposition; Devonian; lamprophyre; Llandoverian; metamorphic rock; muscovite; Silurian; Bergen Arcs; Caledonides; Eurasia; Europe; Northern Europe; Norway; Scandinavia
dc.titleAge constraints on the late Caledonian (Scandian) deformation in the Major Bergen Arc, SW Norway
dc.typeJournal article
local.bibliographicCitation.lastpage70
local.bibliographicCitation.startpage59
local.contributor.affiliationFossen, H, University of Bergen
local.contributor.affiliationDunlap, William James, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidDunlap, William James, u9505456
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040312 - Structural Geology
local.identifier.ariespublicationu9503261xPUB24
local.identifier.citationvolume86
local.identifier.scopusID2-s2.0-33845776589
local.type.statusPublished Version

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