The Pondosa fault zone: A distributed dextral-normal-oblique fault system in northeastern California, USA

Geosphere
By: , and 

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Abstract

The tectonic domains of Basin and Range extension, Cascadia subduction zone contraction, and Walker Lane dextral transtension converge in the Mushroom Rock region of northeastern California, USA. We combined analysis of high-resolution topographic data, bedrock mapping, 40Ar/39Ar geochronology, low-temperature thermochronology, and existing geologic and fault mapping to characterize an extensive dextral-normal-oblique fault system called the Pondosa fault zone. This fault zone extends north-northwest from the Pit River east of Soldier Mountain, California, into moderately high-relief volcanic topography as far north as the Bartle (California) townsite with normal and dextral offset apparent in geomorphology and fault exposures. New and existing 40Ar/39Ar and radiocarbon dating of offset lava flows provides ages of 12.4 ka to 9.6 Ma for late Cenozoic stratigraphic units. Scarp morphology and geomorphic expression indicate that the fault system was active in the late Pleistocene. The Pondosa fault zone may represent a dextral-oblique accommodation zone between north-south–oriented Basin and Range extensional fault systems and/or part of the Sierra Nevada–Oregon Coast block microplate boundary.

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Publication type Article
Publication Subtype Journal Article
Title The Pondosa fault zone: A distributed dextral-normal-oblique fault system in northeastern California, USA
Series title Geosphere
DOI 10.1130/GES02450.1
Volume 19
Issue 1
Publication Date December 07, 2022
Year Published 2022
Language English
Publisher Geological Society of America
Contributing office(s) Geologic Hazards Science Center - Seismology / Geomagnetism
Description 27 p.
First page 179
Last page 205
Country United States
State California
Other Geospatial eastern California
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