Flysch and associated beds of the Martinsburg Formation (Ordovician), central Appalachians

作者: Earle F. Mcbride

DOI: 10.1306/74D70C45-2B21-11D7-8648000102C1865D

关键词: PaleocurrentGraded beddingGeologyPlutonPaleontologyMetamorphic rockFlyschSedimentary rockTurbidity currentOrdovician

摘要: … Graded bedding, sole marks, intraformational shale fragments, convolute and small-scale cross-lamination of the flysch-type Martinsburg graywackes suggest a turbidity current origin. …

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