Abstract
IN some districts it seems that iron pyrites formed an important constituent during the deposition of the Magnesium Limestone—not only in the north of England, but in America also in some of the Magnesium Limestones of the Cambrian age.
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ABBOTT, G. Cavities due to Pyrites in Magnesium Limestone. Nature 95, 395 (1915). https://doi.org/10.1038/095395b0
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DOI: https://doi.org/10.1038/095395b0
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