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24 April 2024
 
  » pubmed » pmid17755032

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Cristobalitic Stage in the Diagenesis of Diatomaceous Shale
K J Murata ; J K Nakata ;
Date 3 May 1974
Journal Science, 184 (4136), 567-568
AbstractWith increasing depth of burial, diagenetic cristobalite in the Monterey Shale of California shows a decrease in the d(101) spacing from 4.115 to 4.040 angstroms, indicative of a progressive change in its internal structure. The spacing is 0.004 to 0.015 angstrom smaller in porcellanite than in associated chert, probably because the cristobalite of porcellanite formed later than that of chert.
Source PubMed, pmid17755032 doi: 10.1126/science.184.4136.567
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