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Journal of Sedimentary Petrology
Vol. 39 (1969)No. 4. (December), Pages 1616-1618
Iron-bearing Heavy Minerals in the Sespe Formation (California): NOTES
Ronald C. Flemal
The original detrital iron-bearing heavy minerals of the Sespe Formation have been altered to a hematiteleueoxene suite. Most of this alteration must have occurred after deposition and some iron mobility may still be present.
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