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American Mineralogist; April 1994; v. 79; no. 3-4; p. 397-400
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Significance of magnesite paragenesis in ultrahigh-pressure metamorphic rocks

R. Y. Zhang, and J. G. Liou

Stanford University, Department of Geological and Environmental Sciences, Stanford, CA, United States

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In situ X-ray observation of the reaction dolomite = aragonite + magnesite at 900-1300 K
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