On the ophiolite of Thurman, Warren County, New York, with remarks on the Eozoon canadense.
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Abstract
THE Warren Oounty Ophiolite or Verdantique Marble as seen in the limited amount put upon the market, consists in its typical development of an even grallular admixture of white calcite and pale yellowish green serpentine in about equal proportions.The uniformity of texture is, however, often interrupted by large irregular blotches of deep lustrous green ser• pentine which, as shown in a large block in the National * Renard mentions grains of palagonite in a fragmental rock collected by Bnchanan on Rat Island, loco cit., p. 11.
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| Authors | George P. Merrill |
| Journal | american journal of science |
| Year | 1889 |
| DOI |
10.2475/ajs.s3-37.219.189
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| URL | |
| Keywords | Keywords not found |
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