Retrograde pumpellyite in the Yunotani garnet blueschist of the Omi area, Japan: An update on the cooling path
Author:
Affiliation:
1. Department of Earth Science, Tohoku University
2. Center for Northeast Asian Studies, Tohoku University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/114/1/114_180716/_pdf
Reference39 articles.
1. Beiersdorfer, R.E. and Day, H.W. (1995) Mineral paragenesis of pumpellyite in low–grade mafic rocks. Geological Society of America Special Paper, 296, 5–27.
2. Carpenter, M.A. (1980) Mechanisms of exsolution in sodic pyroxenes. Contributions to Mineralogy and Petrology, 71, 289–300.
3. de Capitani, C. and Petrakakis, K. (2010) The computation of equilibrium assemblage diagrams with Theriak/Domino software. American Mineralogist, 95, 1006–1016.
4. Ernst, W.G. (1988) Tectonic history of subduction zones inferred from retrograde blueschist P–T paths. Geology, 16, 1081–1084.
5. Ernst, W.G. and Peacock, S.M. (1996) A thermotectonic model for preservation of ultrahigh–pressure phases in metamorphosed continental crust. In Subduction, Top to Bottom (Bebout, G.F., Scholl, D.W., Kirby, S.H. and Platt, J.P. Eds.). Geophysical Monograph 96, American Geophysical Union, Washington, D.C., 171–178.
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