Particle mixing rates in deep-sea sediments determined from excess 210Pb and 32Si profiles
- 1 December 1982
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 61 (2) , 257-271
- https://doi.org/10.1016/0012-821x(82)90057-7
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Radium, thorium, uranium, and 210 Pb in deep-sea sediments and sediment pore waters from the North Equatorial PacificAmerican Journal of Science, 1980
- Measurement of theHalf-Life via Accelerator Mass SpectrometryPhysical Review Letters, 1980
- The half life of32Si determined from a varved Gulf of California sediment coreEarth and Planetary Science Letters, 1980
- Tests for size and shape dependency in deep-sea mixingSedimentary Geology, 1980
- Quantitative effects of sediment mixing on stratigraphy and biogeochemistry: a signal theory approachNature, 1977
- The electrodeposition and determination of radium by isotopic dilution in sea water and in sediments simultaneously with other natural radionuclidesAnalytica Chimica Acta, 1975
- North American microtektites from the Caribbean Sea and their fission track ageEarth and Planetary Science Letters, 1973
- Reworking of deep-sea sediments as indicated by the vertical dispersion of the Australasian and ivory coast microtektite horizonsEarth and Planetary Science Letters, 1969
- Comparison of sedimentation rates obtained by32Si and uranium decay series determinations in some siliceous Antarctic coresEarth and Planetary Science Letters, 1969
- Cosmic-Ray-Produced Silicon-32 in NatureScience, 1960