Geophysical study of Cenozoic geologic structures of northern Owens Valley, California

Geophysics
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Abstract

A narrow gravity minimum anomaly of amplitude 30 mgals indicates that northern Owens ValleyCalifornia, a narrow fault-bounded trough or graben filled with Cenozoic clastic deposits to a depth of as much as 8,000 ft. Seismic-refraction measurements support this conclusion. Aeromagnetic and gravity measurements define a small, dense, and magnetic body buried by the valley fill of northern Owens Valley

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Publication type Article
Publication Subtype Journal Article
Title Geophysical study of Cenozoic geologic structures of northern Owens Valley, California
Series title Geophysics
DOI 10.1190/1.1439021
Volume 27
Issue 3
Year Published 1962
Language English
Publisher Society of Exploration Geophysicists
Description 9 p.
First page 334
Last page 342
Country United States
State California
Other Geospatial Owens Valley
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