Aerial view of the Queen Valley and Coaldale faults at the northern end of White Mountains. Photo by D. Stockli triangular facet Sierra Nevada normal fault, Onion Creek.

Late Cenozoic Intraplate Deformation in the Eastern California Shear Zone-Walker Lane Belt

Project Summary

The research focus of these collaborative NSF funded projects centers on the kinematics and active tectonics of the northern part of the Eastern California Shear Zone and southern Walker Lane Belt. These two regions straddle a complex zone—the boundary between dominantly east-west extension in the Basin and Range Province to the east and dominantly NW-dextral shear along the Pacific-North American plate boundary to the west. The interaction between extension and transcurrent shear has resulted in the development of a complex array of faults that accommodate intraplate strain.

Our field-based research, combined with tectonic geomorphology, paleoseismology, thermochronology, and geochronology investigations, focuses on two regions. The first region is the northern part of the Eastern California Shear Zone where we are investigating the kinematics and active tectonics of a system of intraplate dextral and normal faults. The second region is the southern Walker Lane Belt, known as the Mina deflection, where we are studying the kinematics and active tectonics of an integrated system of dextral, sinistral, and normal faults. Our research on the spatial and temporal patterns of strain release during late Cenozoic to Recent times is motivated in large part by ongoing geodetic investigations on present-day magnitude of strain accumulation and patterns of strain distribution across the Eastern California Shear Zone and Walker Lane Belt. Furthermore, data sets from both regions will provide important constraints on geodynamic hypotheses proposed for the evolution of the Eastern California Shear Zone and Walker Lane Belt. An accurate characterization of the temporal and spatial strain distribution within the Eastern California Shear Zone and Walker Lane Belt is crucial for understanding tectonic processes over a much broader area of intraplate deformation associated with the interaction between the Pacific and North American plates.

Research collaborators include: Lewis Owen (University of Cincinnati), Bob Finkel (Lawrence Livermore Lab), John Oswald (Scotia Pacific Company), Andy Calvert (USGS), Charlie Rubin (CWU), Danny Stockli (Univ. of Kansas), and John Gosse (Dalhousie Univ.).


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