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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In our eReader you can find the full English version of the book. Read An Old Chapter of the Geological Record With a New Interpretation Or Rock Meta Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book 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*.
What to read after An Old Chapter of the Geological Record With a New Interpretation Or Rock Meta?
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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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