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pro vyhledávání: '"Jeffrey W. Bader"'
Autor:
Jeffrey W. Bader
Publikováno v:
The Mountain Geologist. 58:27-37
The North Owl Creek fault is an E–W-striking, basement-rooted Laramide structure located in the Owl Creek Mountains of north-central Wyoming that likely has Precambrian origins. It is defined by a rectilinear zone of deformation that extends eastwa
Autor:
Jeffrey W. Bader
Publikováno v:
Lithosphere. 11:129-148
Publikováno v:
Proceedings of the 9th Unconventional Resources Technology Conference.
Autor:
Jeffrey W. Bader
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Jeffrey W. Bader
Publikováno v:
Rocky Mountain Geology. 44:121-145
The Douglas Creek arch is a north–south-trending faulted anticline that separates the Uinta basin of northeastern Utah from the Piceance basin of northwestern Colorado. Previous work indicates that the arch initially formed during the Laramide orog
Autor:
Jeffrey W. Bader
Publikováno v:
Rocky Mountain Geology. 43:23-40
The Cherokee Ridge arch is an east–west-trending structure that separates the Washakie Basin of south-central Wyoming from the Sand Wash Basin of northwestern Colorado. It is characterized by a distinct east–west-trending lineament on Landsat ima
Autor:
Jeffrey W. Bader
Publikováno v:
Open-File Report.