To use all functions of this page, please activate cookies in your browser.
my.chemeurope.com
With an accout for my.chemeurope.com you can always see everything at a glance – and you can configure your own website and individual newsletter.
 My watch list
 My saved searches
 My saved topics
 My newsletter
Samariumneodymium datingSamariumneodymium dating is useful for determining the age relationships of rocks and meteorites. Sm/Nd ratios are used to provide information on the source of igneous melts as well as to provide age data. The various reservoirs within the solid earth will have different values of initial ^{143}Nd/^{144}Nd ratios, especially with reference to the mantle. Additional recommended knowledgeThe usefulness of SmNd dating is the fact that these two elements are rare earths. They are thus, theoretically, not particularly susceptible to partitioning during melting of silicate rocks. The fractionation effects of crystallisation of felsic minerals (see above) changes the Sm/Nd ratio of the resultant materials. This, in turn, influences the ^{143}Nd/^{144}Nd ratios with ingrowth of radiogenic ^{143}Nd. The mantle is assumed to have undergone chondritic evolution, and thus deviations in initial ^{143}Nd/^{144}Nd ratios can provide information as to when a particular rock or reservoir was separated from the mantle within the Earth's past. In many cases, SmNd and RbSr isotope data is used together. SmNd radiometric datingSamarium has five naturally occurring isotopes and neodymium has seven. ^{146}Sm is an extinct nuclide which decays via alpha emission to produce ^{142}Nd, with a halflife of 1.08 x 10^{8} years. ^{146}Sm is itself produced by the decay of ^{150}Gd via alphadecay with a halflife of 1.06 x 10^{11} years. An isochron is calculated normally. As with RbSr and PbPb isotope geochemistry, the initial ^{143}Nd/^{144}Nd ratio of the isotope system provides important information on crustal formation and the isotopic evolution of the solar system. Sm and Nd geochemistryThe concentration of Sm and Nd in silicate minerals increase with the order in which they crystallise from a magma according to Bowen's reaction series. Samarium is accommodated more easily into mafic minerals, so a mafic rock which crystallises mafic minerals will concentrate neodymium in the melt phase faster relative to samarium. Thus, as a rock undergoes fractional crystallization from a mafic to a more felsic composition, the abundance of Sm and Nd changes, as does the ratio between Sm and Nd. Thus, ultramafic rocks have low Sm and Nd and high Sm/Nd ratios. Felsic rocks have high concentrations of Sm and Nd but low Sm/Nd ratios (komatiite has 1.14ppm Sm and 3.59ppm Nd versus 4.65ppm Sm and 21.6ppm Nd in rhyolite). The importance of this process is apparent in modeling the age of continental crust formation. Crustal segregation modelingThe process of modelling crustal segregation ages work like this; We must assume a chondritic evolution for the Earth. In other words, we assume the Earth is formed from chondritic material, with a Nd/Nd ratio comparable to chondrite meteorites, and with similar bulk Sm/Nd ratio and abundances. Because, as ^{147}Sm decays to ^{143}Nd at a known rate and we know the Sm/Nd ratio and current Nd/Nd ratio of the chondrites, the chondritic uniform reservoir (CHUR) initial Nd/Nd ratio can be mathematically modelled for any point in time. For certain assumptions CHUR is assumed to represent the mantle. We take a rock, for example a granulite from the lower continental crust, and measure the Sm and Nd elemental abundances, and the abundances of isotopes of these elements within the rock. We can then calculate the presentday ^{147}Sm:^{143}Nd ratio and the current ^{143}Nd/^{144}Nd ratio. This can derive a radiometric age of the rock. We can then mathematically calculate, given the current ^{143}Nd/^{144}Nd ratio and Sm:Nd elemental ratio of the granulite, an age at which the granulite ^{143}Nd/^{144}Nd ratio was equivalent to the CHUR ^{143}Nd/^{144}Nd ratio. This calculation derives a time at which, hypothetically, the granulite could have been formed from the assumed reservoir by a melting event. This is known as the segregation age.


This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Samariumneodymium_dating". A list of authors is available in Wikipedia. 