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Sm–Nd Dating

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Encyclopedia of Scientific Dating Methods

Definition

Samarium–neodymium dating uses the radioactive decay of 147Sm to 143Nd and 146Sm to 142Nd to measure the age of rocks and minerals and to trace and date geochemical processes responsible for the chemical differentiation of the Earth and the terrestrial planets and planetesimals.

Introduction

Introduced to the geochemical and cosmochemical communities in the early 1970s, the Sm–Nd radioactive decay systems have grown into essential tools in geochronology and particularly for the tracing of geochemical processes. A key strength of Sm–Nd dating is that it involves two rare earth elements (REE). The behavior of the REE during geologic processes is relatively well understood because, with the exception of Eu and Ce under some conditions, they all have the same ionic charge of +3 and their ionic radius changes monotonically as a function of atomic number. As a result, their fractionation from one another during silicate rock melting and crystallization is predictable. In addition,...

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Carlson, R.W. (2013). Sm–Nd Dating. In: Rink, W., Thompson, J. (eds) Encyclopedia of Scientific Dating Methods. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6326-5_84-1

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