Shelf, paralic, and fluvial environments and eustatic sea-level fluctuations in the origin of the Tuscarora Formation (Lower Silurian) of central Pennsylvania | Citedby Results | Journal of Sedimentary Research | GeoScienceWorld

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Shelf, paralic, and fluvial environments and eustatic sea-level fluctuations in the origin of the Tuscarora Formation (Lower Silurian) of central Pennsylvania

Journal of Sedimentary Research (1983) 53 (1): 25–49.

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