Age Determination of Pacific Chalk Ooze by Radiocarbon and Titanium Content
Open Access
- 1 November 1951
- journal article
- Published by Stockholm University Press in Tellus
- Vol. 3 (4) , 222-229
- https://doi.org/10.1111/j.2153-3490.1951.tb00803.x
Abstract
Measurements have been carried out on the average radiocarbon activity of a sediment core of eupelagic chalk ooze and the age of the lower boundary was calculated by integration of the radiocarbon decay function. In such cores where constancy of the rate of minerogenous accumulation is indicated and can be checked by lateral control, the titanium content, calibrated in terms of absolute age by means of radiocarbon measurement, can be used for dating as far back in time as the constancy of the rate of minerogenous sedimentation can be proved. DOI: 10.1111/j.2153-3490.1951.tb00803.xKeywords
This publication has 22 references indexed in Scilit:
- Radiocarbon Datability of Peat, Marl, Caliche , and Archaeological MaterialsScience, 1951
- Measurement of Low Level RadiocarbonReview of Scientific Instruments, 1951
- Radiocarbon DatesScience, 1951
- World-Wide Distribution of Natural RadiocarbonPhysical Review B, 1951
- The Swedish Deep Sea Expedition. The Geological Material and its Treatment with special Regard to the Eastern PacificGeologiska Föreningen i Stockholm Förhandlingar, 1950
- Late Ceriozoic Climatic Charges as Recorded by the Equatorial Current SystemTellus A: Dynamic Meteorology and Oceanography, 1950
- Age Determinations by Radiocarbon Content: Checks with Samples of Known AgeScience, 1949
- Natural Radiocarbon from Cosmic RadiationPhysical Review B, 1947
- Radiocarbon From Cosmic RadiationScience, 1947
- Die Sedimente des äquatorialen Atlantischen OzeansGeologiska Föreningen i Stockholm Förhandlingar, 1937