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Images (a), (b) and (d) –(f) courtesy of Dr. J. Schieber, Indiana University.
Color cathodoluminescence reveals provenance of populations of quartz grains (a) Cleveland shale (Devonian); low grade metamorphic acadian orogeny; (b) Barnett shale (Miss.) Texas; low grade metamorphic ouchita orogeny; (c) Unspecified; (d) Santa Barbara basin shale (modern); plutonic (Sierra Nev