| Kyanite-Sillimanite Equilibrium at 750{degrees}C. | |
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MedLine Citation:
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PMID: 17800996 Owner: NLM Status: PubMed-not-MEDLINE |
Abstract/OtherAbstract:
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Reversal of the kyanite-sillimanite inversion has been accomplished hydrothermally at 750 degrees C. The inversion pressure at 750 degrees C is 8.1 +/- 0.4 kilobars. The calculated pressuretemperature slope at this point is 17.7+/- 1.0 bars per degree celsius. Geologically, this result seems more plausible than previous estimates of the location of the boundary. When combined with other work on the relative stability of andalusite, the data indicate that andalulsite cannot be stable at a pressure greater than 4.2 kilobars. |
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Authors:
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R C Newton |
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Publication Detail:
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Type: Journal Article |
Journal Detail:
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Title: Science (New York, N.Y.) Volume: 151 ISSN: 0036-8075 ISO Abbreviation: Science Publication Date: 1966 Mar |
Date Detail:
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Created Date: 2010-06-07 Completed Date: 2010-07-02 Revised Date: - |
Medline Journal Info:
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Nlm Unique ID: 0404511 Medline TA: Science Country: United States |
Other Details:
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Languages: eng Pagination: 1222-5 Citation Subset: - |
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From MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine
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