. Preliminary well site observation has determined that most of the core showed
100% moderately bright yellow natural fluorescence with a slow streaming weak pale
blue blooming to diffuse cut and a moderately thin to thick pale blue residual ring. The
majority of the core appeared to be sandstone with a trace of siltstone, very fine
grained to coarse grained with a well developed siliceous cement, rare matrix,
. Preliminary well site observation has determined that most of...
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