Natural radioisotope210Pb as an indicator of origin of fine-grained sediment
Distribution of210Pb in sediments on the South Texas Continental Shelf is related to dynamics of the sedimentary transport processes. This radioisotope, whose concentration is time-dependent, defines three depocenters on the shelf. In addition, the variation of210Pb activity at the sediment/water interface delineates areas of terrigenous sedimentation from hemipelagic sedimentation. ?? 1985 Springer-Verlag New York Inc.
Citation Information
| Publication Year | 1984 |
|---|---|
| Title | Natural radioisotope210Pb as an indicator of origin of fine-grained sediment |
| DOI | 10.1007/BF02281706 |
| Authors | C. Holmes |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Geo-Marine Letters |
| Index ID | 70013953 |
| Record Source | USGS Publications Warehouse |