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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.
Citation Information
Publication Year
1975
Title
Silica mineralogy and structure of the Monterey Shale, Temblor Range, California