This mineral, Baddeleyite usually occurs as black botryoidal crystals or brown-yellow micro blades. In this specimen the Baddeleyite occurs as a staw-yellow parallel layered crystal that runs all through the dark red hematite. Nothing like we've seen elsewhere. The wine red is hematite, and there's also some micro quartz and calcite in there as well. You can actually read about this find in Vol 37 Iss. 1 of the Mineralogical Record, in an article about the Francon Quarry by Dr. Tarassoff. He collected the specimen in 1976.
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