Geophysical study of Cenozoic geologic structures of northern Owens Valley, California
Geophysics
By: L. C. Pakiser and M. F. Kane
Links
- More information: Publisher Index Page (via DOI)
- Download citation as: RIS | Dublin Core
Abstract
A narrow gravity minimum anomaly of amplitude 30 mgals indicates that northern Owens Valley, California, 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.
Suggested Citation
Pakiser, L.C., Kane, M.F., 1962, Geophysical study of Cenozoic geologic structures of northern Owens Valley, California: Geophysics, v. 27, no. 3, p. 334-342, https://doi.org/10.1190/1.1439021.
Study Area
| 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 |