Geology of clays

@inproceedings{Millot1970GeologyOC,
  title={Geology of clays},
  author={Georges Millot and William R. Farrand and H{\'e}l{\`e}ne Paquet and Lowell A. Douglas},
  year={1970}
}

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References

SHOWING 1-5 OF 5 REFERENCES

Genesis of Clay Minerals: Inheritance and Transformation

Throughout the expose of facts three principal processes have been invoked to account for the genesis of clay minerals: Detrital inheritance; Transformations; Neoformations.

Superficial Geochemistry and The Silicate Cycle

By a slow process clays have been described in their deposits and then in the mechanisms of their formation. It is instructive at the end of this process to consider the whole problem in geochemical

Conclusions: Inheritance and transformations by addition and subtraction 322

    The silicate cycle: Metamorphism of clay minerals. Convergence and divergence of the geochemical cycles of elements

      283 -Geological and petrographic data: Climatic silicification. -Flint, cherts and silicifications of sedimentary rocks