Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf.
Geologie en Mijnbouw
By: C.H. Nelson
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Abstract
The distribution of late Pleistocene and Holocene surface sediments on the northern Bering Seafloor is patchy and dependent upon locations of seafloor bedrock and pre-late Pleistocene glacial debris, late Holocene river sediment influx, and modern strong bottom currents. Seafloor vibracores and high-resolution profiles record two different sedimentary environments in the northern Bering shelf: late Pleistocene-Holocene shoreline transgression in Chirikov Basin, and Holocene deposition from the Yukon River in Norton Sound.-from Author
Suggested Citation
Nelson, C., 1982, Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf.: Geologie en Mijnbouw, v. 61, no. 1, p. 5-18.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf. |
| Series title | Geologie en Mijnbouw |
| Volume | 61 |
| Issue | 1 |
| Year Published | 1982 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Geologie en Mijnbouw |
| First page | 5 |
| Last page | 18 |