Ronald C. Flemal; Iron-bearing heavy minerals in the Sespe Formation (California). Journal of Sedimentary Research ; 39 (4): 1616–1618. doi: https://doi.org/10.1306/74D71EBF-2B21-11D7-8648000102C1865D
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The original detrital iron-bearing minerals of the Sespe Formation have been altered to a hematite-leucoxene suite. Most of this alteration must have occurred after deposition and some iron mobility may still be present.
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