An Old Chapter of the Geological Record With a New Interpretation Or Rock Meta
An Old Chapter of the Geological Record With a New Interpretation Or Rock Meta
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OPHITES AND RELATED ROCKS. 21 evidence that thermal waters aided the assumed chemical reactions.
Having now disposed of all the serpentinous structures of " Eozoon Canadense " in strict conformity with the mutations known to characterize the minerals composing them, we shall next offer our explanation of the origin of the calcitic layers which form the " intermediate skeleton " of this reputed fossil.
With respect to the interchanges between a mineral silicate and a mineral carbonate, often obt...aining in ophite, we find that the calcite which frequently holds a place in the layers of chry- sotile is fibrous in certain instances, and retains the original structure of the latter mineral. Generally, however, the charac- teristic rhombohedral cleavage of calcite is developed. This replacement of chrysotile by a mineral carbonate retaining its typical fibrosity, and therefore possessing a fibrous structure similar to that of aragonite, has occurred to us in specimens of ophi-euphotide from the north of Italy, as already noticed in one of our previous memoirs*.
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To quickly assess the difficulty of the text, read a short excerpt:
OPHITES AND RELATED ROCKS. 21 evidence that thermal waters aided the assumed chemical reactions.
Having now disposed of all the serpentinous structures of " Eozoon Canadense " in strict conformity with the mutations known to characterize the minerals composing them, we shall next offer our explanation of the origin of the calcitic layers which form the " intermediate skeleton " of this reputed fossil.
With respect to the interchanges between a mineral silicate and a mineral carbonate, often obt...aining in ophite, we find that the calcite which frequently holds a place in the layers of chry- sotile is fibrous in certain instances, and retains the original structure of the latter mineral. Generally, however, the charac- teristic rhombohedral cleavage of calcite is developed. This replacement of chrysotile by a mineral carbonate retaining its typical fibrosity, and therefore possessing a fibrous structure similar to that of aragonite, has occurred to us in specimens of ophi-euphotide from the north of Italy, as already noticed in one of our previous memoirs*.
What to read after An Old Chapter of the Geological Record With a New Interpretation Or Rock Meta?
You can find similar books in the "Read Also" column, or choose other free books by W William King to read onlineMoreLess
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