Interfacial energies of quartz/quartz (qz/qz), albite/albite (ab/ab), and quartz/albite (qz/ab) boundaries in low-grade pelitic schist were determined based on measured values of dihedral angles. Three kinds of microstructures were investigated, and the interfacial energies were obtained in two independent ways. (1) Relative values of interfacial energy were calculated from dihedral angles formed at quartz and albite triple junctions. (2) Subgrain boundary energy was calculated using the Read-Shockley theory for a boundary connected to an intergranular pore. Dihedral angles formed at the corners of intergranular pores were measured. From the interfacial tension balance equation, the value of the qz/qz grain boundary energy was then obtained. (3) Dihedral angles formed at intersections of either pericline or albite twin boundaries with either ab/ab or qz/ab boundaries were measured. The twin boundary energy was calculated based on a previously derived equation using Landau potential, twin wall thickness, and critical temperature for a phase transition in albite. With a modified interfacial tension balance equation for a twin boundary fixed to a facet orientation, the interfacial energies of ab/ab and qz/ab boundaries were obtained. Energies obtained by methods of (2) and (3) are in good agreement. The interfacial energies for qz/qz, ab/ab, and qz/ab boundaries obtained in this study are 270 ∓ 110, 300 ∓ 150, and 250 ∓ 120 mJ/m2, respectively.
|Original language||English (US)|
|Number of pages||9|
|Journal||Contributions to Mineralogy and Petrology|
|State||Published - Sep 2002|
Bibliographical noteFunding Information:
Acknowledgements This research was funded by a JSPS Postdoctoral Fellowship for Research Abroad and the NSF through grant EAR-0126277. E.L.K. Salje and S.A Hayward are gratefully acknowledged for the derivation of the twin boundary energy. We thank M. Shiba for helping to collect our samples. M. Holness and an anonymous reviewer are acknowledged for helpful and constructive comments.