Investigating the Paleozoic-Mesozoic low-temperature thermal history of the southwestern Canadian Arctic: insights from (U-Th)/He thermochronology

The Arctic Amerasia Basin, located between the Canadian margin and Alaska, formed by purported Jurassic–Cretaceous rifting related to the rotation of the Arctic Alaska – Chukotka microcontinent from northern Laurentia. Rifting may have been accompanied by rift shoulder uplift and cooling that is rec...

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Bibliographic Details
Main Authors: Midwinter, Derrick, Powell, Jeremy, Schneider, David, Dewing, Keith
Format: Article in Journal/Newspaper
Language:unknown
Published: NRC Research Press (a division of Canadian Science Publishing) 2016
Subjects:
Online Access:http://hdl.handle.net/1807/75886
http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2016-0088