Strain accumulation across the Wasatch Fault near Ogden, Utah

Journal of Geophysical Research B: Solid Earth
By: , and 

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Abstract

Deformation of a 70 by 40‐km trilateration network spanning the north trending Wasatch fault near Ogden, Utah, has been monitored from 1972 through 1990. All but nine of the 200 measurements are consistent with deformation that is linear in time. We presume that those nine observations are contaminated by some blunder in making the measurements and that deformation is linear in time. The strain rate over the 1972–1990 interval across a 40‐km‐wide zone west of the Wasatch fault (hanging wall block) is adequately approximated by a 0.04 ± 0.01 μstrain/yr N85°E±5° uniaxial extension. Adequate coverage of the footwall block is available only over the 1981–1990 interval, and the strain rate across a 30‐km‐wide zone there is approximated by a 0.07 ± 0.03 μstrain/yr N20°E±12° uniaxial extension. The observed extension of the hanging wall block in the direction normal to fault strike suggests that the Wasatch fault may be listric; a planar fault would produce a zone of contraction normal to the fault at the surface of the hanging wall block. The component of extension parallel to fault strike observed on the footwall block is unexplained.

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Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Strain accumulation across the Wasatch Fault near Ogden, Utah
Series title Journal of Geophysical Research B: Solid Earth
DOI 10.1029/91JB02798
Volume 97
Issue B2
Year Published 1992
Language English
Publisher American Geophysical Union
Contributing office(s) Earthquake Science Center
Description 13 p.
First page 2071
Last page 2083
Country United States
State Utah
Other Geospatial Wasatch Fault
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