Silica mineralogy and structure of the Monterey Shale, Temblor Range, California

K. J. Murata; R.G. Randall

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USGS · 70156585

Silica mineralogy and structure of the Monterey Shale, Temblor Range, California

K. J. Murata·R.G. Randall

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Abstract

The d (101) spacing of diagenetic cristobalite decreases regularly with depth of burial in the siliceous Monterey Shale of the Temblor Range. This relation has been used to delineate the folded structure of the Monterey Shale at a locality near Taft.

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Journal of Research of the U.S. Geological Survey Article

Source-reported bounding extent: 34.93323032184192° to 36.30627216957992° latitude; -120.63262939453124° to -118.88305664062499° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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K. J. Murata, R.G. Randall. 1975. Silica mineralogy and structure of the Monterey Shale, Temblor Range, California. https://pubs.usgs.gov/publication/70156585

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