1. A Large-scale isotope anomaly in the Southern Hemisphere mantle Stanley R. Hart

2. Figure 14-9. (Winter) From Hart (1984) Nature, 309, 753-756.

3. Can Generate tholeiitic and alkaline basalts from a chemically uniform mantle Variables –Temperature –Pressure Figure 10-2 (Winter) Phase diagram of aluminous lherzolite with melting interval (gray), sub-solidus reactions, and geothermal gradient. After Wyllie, P. J. (1981). Geol. Rundsch. 70, 128-153.

4. Trace Elements: REEs Figure 14-2. (Winter) After Wilson (1989) Igneous Petrogenesis. Kluwer.

5. Isotope Geochemistry Isotopes do not fractionate during partial melting of fractional melting processes, so will reflect the characteristics of the source OIBs, which sample a great expanse of oceanic mantle in places where crustal contamination is minimal, provide incomparable evidence as to the nature of the mantle

6. Pb Isotopes Pb produced by radioactive decay of U & Th 238 U  234 U  206 Pb 235 U  207 Pb 232 Th  208 Pb

7. Pb is quite scarce in the mantle –Mantle-derived melts susceptible to contamination –U, Pb, and Th are concentrated in continental crust (high radiogenic daughter Pb isotopes) – 204 Pb is non-radiogenic, so 208 Pb/ 204 Pb, 207 Pb/ 204 Pb, and 206 Pb/ 204 Pb increase as U and Th decay –Oceanic crust has elevated U and Th content (compared to the mantle) as will sediments derived from oceanic and continental crust –Pb is a sensitive measure of crustal (including sediment) components in mantle isotopic systems

8. Figure 14-8. After Wilson (1989) Igneous Petrogenesis. Kluwer. Data from Hamelin and Allègre (1985), Hart (1984), Vidal et al. (1984).

9. Can map the geographic distribution of the isotopic data Figure 14-9. From Hart (1984) Nature, 309, 753-756.

10. Isotopically enriched reservoirs (EMI, EMII, and HIMU) are too enriched for any known mantle process, and they correspond to crustal rocks and/or sediments EMI (slightly enriched) correlates with lower continental crust or oceanic crust EMII is more enriched, especially in radiogenic Sr (indicating the Rb parent) and Pb (U/Th parents) correlates with the upper continental crust or ocean-island crust

11. A Model for Oceanic Magmatism DM OIB ContinentalReservoirs EM and HIMU from crustal sources (subducted OC + CC seds) Figure 14-10. Nomenclature from Zindler and Hart (1986). After Wilson (1989) and Rollinson (1993).