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1.- OROGENICALLY-DERIVED MIDDLE ORDOVICIAN CLASTIC WEDGE IN THE BROKEN BOW UPLIFT, OUACHITA ALLOCHTHON, OKLAHOMA; A KEY LINK IN THE TACONIAN-FAMATINIAN CONNECTION?
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1995
GEOLOGICAL SOCIETY OF AMERICA, 1995 ANNUAL MEETING
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