Direct determination of the quartz-coesite transition by in situ X-ray measurements
Contributions to Mineralogy and Petrology, ISSN: 0010-7999, Vol: 48, Issue: 2, Page: 149-152
1974
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Article Description
The quartz-coesite transition has been determined over the temperature range 600-1100° C by in Situ X-ray measurements with NaCl as internal pressure standard. An internally heated high-pressure X-ray apparatus ("Belt"-type) was used which is based on the principle developed by Freud and Sclar (1969). The obtained quartz-coesite equilibrium line may be represented by the equation P=31±1+0.0075 T where P is in kb and T in ° C. © 1974 Springer-Verlag.
Bibliographic Details
http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=0013166017&origin=inward; http://dx.doi.org/10.1007/bf00418617; http://link.springer.com/10.1007/BF00418617; http://link.springer.com/content/pdf/10.1007/BF00418617; http://link.springer.com/content/pdf/10.1007/BF00418617.pdf; http://link.springer.com/article/10.1007/BF00418617/fulltext.html; https://dx.doi.org/10.1007/bf00418617; https://link.springer.com/article/10.1007/BF00418617; http://www.springerlink.com/index/10.1007/BF00418617; http://www.springerlink.com/index/pdf/10.1007/BF00418617
Springer Nature
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