Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny
Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny
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In our eReader you can find the full English version of the book. Read Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny 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 Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny
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The frequent presence of veins of serpentine passing, from the central mass of serpentine, out through the surrounding sulphides seems, at first glance, to point definitely to serpentinization after deposition of sulphides. But on closer examination it becomes evident that the serpentine of these veins is often not continuous 24 NEW YORK STATE MUSEUM with that of the central mass, but is separated from it by a faint but sharp marginal line, which materially weakens this evidence.
The presence o...f abundant cracks in the sulphides suggests yield- ing to the expansive force of growing serpentine and^ consequently, the earlier formation of the sulphides. These cracks, however, are not radial around serpentine grains but commonly occur in parallel systems traversing the whole width of sections, without reference to serpentine. Furthermore, it very often happens that, under the strain that has produced these cracks, a core has separated from the adjacent sulphide and the intervening space has been filled with the vein serpentine.
What to read after Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny?
You can find similar books in the "Read Also" column, or choose other free books by Charles Henry Smyth to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The frequent presence of veins of serpentine passing, from the central mass of serpentine, out through the surrounding sulphides seems, at first glance, to point definitely to serpentinization after deposition of sulphides. But on closer examination it becomes evident that the serpentine of these veins is often not continuous 24 NEW YORK STATE MUSEUM with that of the central mass, but is separated from it by a faint but sharp marginal line, which materially weakens this evidence.
The presence o...f abundant cracks in the sulphides suggests yield- ing to the expansive force of growing serpentine and^ consequently, the earlier formation of the sulphides. These cracks, however, are not radial around serpentine grains but commonly occur in parallel systems traversing the whole width of sections, without reference to serpentine. Furthermore, it very often happens that, under the strain that has produced these cracks, a core has separated from the adjacent sulphide and the intervening space has been filled with the vein serpentine.
What to read after Genesis of the Zinc Ores of the Edwards District St Lawrence County Ny?
You can find similar books in the "Read Also" column, or choose other free books by Charles Henry Smyth to read onlineMoreLess
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