Haynes suggested that the Deicke ash was deposited in the region of the eastern belt but because of reworking or removal ... and one near the middle of the Edinburg (Rader and Read, 1989; John T. Haynes, 1993, personal communication).
Title | : | Ordovician K-bentonites of eastern North America |
Author | : | Dennis R. Kolata, Warren D. Huff, Stig M. Bergstrom |
Publisher | : | Geological Society of America - 1996-01-01 |
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