Sm-Nd age of the Stillwater complex and the mantle evolution curve for neodymium

Mathematics – Logic

Scientific paper

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Earth Mantle, Evolution (Development), Neodymium, Samarium, Abundance, Gabbro, Geological Surveys, Rocks

Scientific paper

The Stillwater layered mafic intrusive complex in southern Montana is studied by means of Sm-Nd and Rb-Sr isotope analysis in order to investigate the applicability of Sm-Nd dating to crystallization age determinations of terrestrial mafic rocks and to study the chemical evolution of the mantle. Internal isochrons determined for samples ranging from anorthosite through gabbro to pyroxenite by the Sm-Nd method indicate an age of 2701 + or - 8 million years, while results of Rb-Sr isotopic measurements show more recent disturbances. The Nd-143/Nd-144 value obtained (0.508248) is found to deviate substantially from the chondritic uniform reservoir evolution curve, implying either early mantle layering with substantial REE fractionation, or REE contamination from older continental crust. It is concluded that the Sm-Nd system appears to be sufficiently resistant to weak metamorphic events to allow the precise dating of ancient terrestrial rocks.

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