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 |
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Title | Natural radioisotope210Pb as an indicator of origin of fine-grained sediment |
DOI | 10.1007/BF02281706 |
Authors | C. W. Holmes |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geo-Marine Letters |
Index ID | 70013953 |
Record Source | USGS Publications Warehouse |