The generation and evolution of the continental crust

@article{Hawkesworth2010TheGA,
  title={The generation and evolution of the continental crust},
  author={C. Hawkesworth and B. Dhuime and A. Pietranik and P. Cawood and A. Kemp and C. Storey},
  journal={Journal of the Geological Society},
  year={2010},
  volume={167},
  pages={229 - 248}
}
  • C. Hawkesworth, B. Dhuime, +3 authors C. Storey
  • Published 2010
  • Geology
  • Journal of the Geological Society
  • Abstract: The continental crust is the archive of the geological history of the Earth. Only 7% of the crust is older than 2.5 Ga, and yet significantly more crust was generated before 2.5 Ga than subsequently. Zircons offer robust records of the magmatic and crust-forming events preserved in the continental crust. They yield marked peaks of ages of crystallization and of crust formation. The latter might reflect periods of high rates of crust generation, and as such be due to magmatism… CONTINUE READING
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    References

    SHOWING 1-10 OF 163 REFERENCES
    Evolution of the continental crust
    • 429
    • Highly Influential
    • PDF
    The differentiation and rates of generation of the continental crust
    • 90
    The growth of continental crust
    • 224
    Apparent episodic crustal growth arising from a smoothly evolving mantle
    • 65
    The geochemical evolution of the continental crust
    • 2,914
    • Highly Influential
    Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon
    • 527
    • Highly Influential
    • PDF
    Evolution of the Archaean crust by delamination and shallow subduction
    • 166