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(1999)The Cambrian-Ordovician boundary beds of the Moscow syneclise contain three acritarch assemblages; one of them is from the uppermost part of the Upper Cambrian (UC4B-1) and the other two from the lower Tremadocian (OT1 and ...
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(2002)This study is to clarify the geologic time of the Dumugol Formation in the Tanyang area on the basis of conodonts. A total of 245 identifiable conodonts were recovered from 56 samples. They are classified ...
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