Ductile deformation and development of andalusite microstructures in the Hongusan area: Constraints on the metamorphism and tectonics of the Ryoke Belt
Author:
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1440-1738.2007.00603.x/fullpdf
Reference37 articles.
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2. Metamorphic conditions of staurolite schists of the Ryoke metamorphic belt in the Hazu-Hongusan area, central Japan;Asami;Journal of the Geological Society of Japan,1982
3. Precise determinations of the equilibria kyanitesillimanite and kyaniteandalusite and a revised triple point for Al2SiO5 polymorphs;Bohlen;American Mineralogist,1991
4. Thermal stability and standard thermodynamic properties of synthetic 2M1-Muscovite, KAl2[AlSi3O10 (OH)2];Chatterjee;Contributions to Mineralogy and Petrology,1974
5. The development of fringe folds during simple shear deformation and their use as kinematic indicators;Grasemann;Journal of Structural Geology,2001
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