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TitleOrigin of the Northeast Alaskan Orocline
AuthorLane, L SORCID logo
SourceProceedings of GeoConvention 2014 FOCUS; 2014 p. 1-2
Alt SeriesEarth Sciences Sector, Contribution Series 20140069
PublisherCanadian Society of Petroleum Geologists
MeetingGeoConvention 2014 FOCUS; Calgary; CA; May 12-16, 2014
Mediaon-line; digital
File formatpdf
NTS107B/03; 107B/04; 107B/05; 107B/06; 107B/11; 107B/12; 107B/13; 107B/14; 107C/03; 107C/04; 107C/05; 107C/06; 107A/01; 107A/02; 107A/07; 107A/08; 107A/09; 107A/10; 107A/15; 107A/16; 107D/01; 107D/02; 107D/07; 107D/08
AreaAlaska; Beaufort Sea; Mackenzie River; Canada; United States of America
Lat/Long WENS-138.0000 -134.0000 69.5000 68.0000
Subjectstectonics; tectonic interpretations; tectonic evolution; tectonic setting; oroclines; Alaskan Orocline; Cretaceous; Mesozoic; Cenozoic; Tertiary
Illustrationslocation maps
ProgramGEM: Geo-mapping for Energy and Minerals Yukon Sedimentary Basins
Abstract(available in French only)
L'oroclinal du nord-est de l'Alaska est une entité du Crétacé terminal-Tertiaire précoce qui s'est formée par l'interaction complexe de forces tectoniques lointaines et de conditions aux limites locales.
Summary(Plain Language Summary, not published)
This abstract summarizes the complex interplay of local boundary conditions and far field tectonic influences that led to the development of the arcuate fold and fault trends that define the northeastern Brooks Range, Beaufort foldbelt and north Yukon fold complex.

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