| 词条 | Draft:Oregon Rotation |
| 释义 |
Oregon rotation is a motion of the earth's crust around the U.S. state of Oregon, inferred from geodesy, paleomagnetism and other measurements. The Oregon Coast Range fault block rotates around a point in Washington State.{{sfn | Orr | Orr | 2012 | p= 217}} The rotational geologic pole for right-lateral faults and seismicity lineations in western Washington and Oregon is {{coord|47.9|N|117.7|W}}{{sfn|Tectonics|2017}} ReferencesSources
|first1=Tom |last1=Brocher |first2=Ray E |last2=Wells |first3=Andrew P. |last3= Lamb |first4=Craig S. |last4=Weaver |journal=Tectonics |date=April 2017 |DOI= 10.1002/2016TC004223 |url=https://www.researchgate.net/publication/315962928_Evidence_for_Distributed_Clockwise_Rotation_of_the_Crust_in_the_Northwestern_United_States_from_Fault_Geometries_and_Focal_Mechanisms_Clockwise_Rotation_in_the_NW_US|ref={{harvid|Tectonics|2017}}}}
| last=Orr | first=Elizabeth L. | last2=Orr | first2=William N. | title=Oregon Geology | publisher=Oregon State University Press | year=2012 | isbn=978-0-87071-682-9 | url=https://books.google.com/books?id=JdUjfL24ixUC | ref=harv }}Category:Geology of Oregon |
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