Holness, M. B. (2010) Decoding dihedral angles in melt-bearing and solidified rocks. Journal of the Virtual Explorer, 35 (2). ISSN 1441-8142 DOI 10.3809/jvirtex.2011.00265Full text not available from this repository.
The dihedral angle is the angle subtended between two grain boundaries at a three-grain junction, or the angle between the two liquid-solid interfaces at the corner of a fluid-filled pore. In textural equilibrium the dihedral angle defines the topology, interconnectivity and amount of a liquid phase. Complete textural equilibrium (in terms of uniform grain size, constant mean curvature of grain boundaries and balancing of interfacial energies at all three- and four-grain junctions) is rare in geological materials, particularly in the crust. Local equilibrium at grain junctions (manifest as dihedral angles) is generally seen in monomineralic rocks, in high-grade metamorphic rocks and in the mantle. The distribution of true dihedral angles, as measured using a universal stage, has great potential use in interpretation of rock history. The studies of disequilibrium dihedral angles are currently at the descriptive stage, and further efforts need to be applied to deriving a quantitative understanding of the processes by which, and rates at which, they attain equilibrium.
|Uncontrolled Keywords:||2011AREP; IA62;|
|Subjects:||05 - Petrology - Igneous, Metamorphic and Volcanic Studies|
|Divisions:||05 - Petrology - Igneous, Metamorphic and Volcanic Studies|
|Journal or Publication Title:||Journal of the Virtual Explorer|
|Depositing User:||Sarah Humbert|
|Date Deposited:||22 May 2012 14:18|
|Last Modified:||23 Jul 2013 10:04|
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