A narrow gravity minimum anomaly of amplitude 30 mgals. indicates that northern Owens Valley is a narrow fault-bounded trough or graben filled with Cenozoic clastic deposits to a depth of as much as 8000 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.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.