Crustal Age Domains and the Evolution of the Continental Crust in the Mozambique Belt of Tanzania: Combined Sm–Nd, Rb–Sr, and Pb–Pb Isotopic Evidence

@article{Mller1998CrustalAD,
  title={Crustal Age Domains and the Evolution of the Continental Crust in the Mozambique Belt of Tanzania: Combined Sm–Nd, Rb–Sr, and Pb–Pb Isotopic Evidence},
  author={A. M{\"o}ller and K. Mezger and V. Schenk},
  journal={Journal of Petrology},
  year={1998},
  volume={39},
  pages={749-783}
}
  • A. Möller, K. Mezger, V. Schenk
  • Published 1998
  • Geology
  • Journal of Petrology
  • African reworking. Eclogite-facies metapelites of the Early Prot- Mozambique Belt; Sr‐Nd‐Pb isotopes erozoic Usagaran Belt likewise exhibit Archean Nd model ages, but higher Pb isotopic ratios are consistent with last recrystallization of feldspar at 2 Ga. Granulites with Nd model ages from 1 to 1·5 Ga only occur in NE Tanzania; because of their restricted range INTRODUCTION in Pb isotopic composition they are interpreted as juvenile additions The study of ancient high-grade gneiss belts… CONTINUE READING
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