Thermo Finnigan Multi-Collector Magnetic Sector Thermal Ionization Mass Spectrometer

This instrument was used to make the first discoveries of isotopic anomalies in Nd and W due to the now extinct 146Sm (half-life = 100 million years) and 182Hf (half-life = 9 million years).
These discoveries resulted in the first age dates of the formation of the Earth's earliest crust (~100 million years after Solar System formation) and its core (formed within 30 million years of Solar System formation.)
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MEASUREMENT EXAMPLES

Professor Stein Jacobsen | EPS Home | Harvard University