HR: 1340h
AN: MR23B-1327    [Abstracts]
TI: The geometry of random mixing: quantifying spatial distributions
AU: Stunitz, H
EM: holger.stuenitz@unibas.ch
AF: Basel University, Geological Institute, Bernoullistr. 32, Basel, CH-4056, Switzerland
AU: * Heilbronner, R
EM: renee.heilbronner@unibas.ch
AF: Basel University, Geological Institute, Bernoullistr. 32, Basel, CH-4056, Switzerland
AU: Schaeben, H
EM: schaeben@geo.tu-freiberg.de
AF: TU Bergakademie Freiberg, Institut fªr Geologie, Bernhard-von-Cotta-Str. 2, Freiberg, D- 09596, Germany
AB: There are a number of deformation mechanisms that involve mixing of particles of different phases. For example, in cataclastic flow, particles are fragmented and displaced past each other, in diffusion creep, grains of one phase nucleate and grow between grains of other phases. The resulting mixtures may form "random", "clustered" or "anticlustered" patterns. To derive the nature of the underlying process and to identify the active deformation mechanisms, it is necessary to find reliable descriptors by which random and non-random spatial distributions can be quantified and distinguished from one another. As an example of a non-random distribution of grains we studied the eclogites of the Troms Nappe (Caledonides, Norway). Previous studies indicate that the dominant deformation mechanism is diffusion creep, a process known to create anticlustered distributions of mineral grains. In the course of field observations we collected a large dataset of random and non-random 2-D geometries and compared it to results from 3-D numerical modelling. Starting with the Markov Chain analysis by Kretz (1970) we formulated two models for random spatial distributions: one based on the relative amount of grain boundary surface (surface model) and one based on the relative volume fraction of each phase (volume model). In both cases, if the aggregate consists of two phases (A and B), the relative amounts of grain contacts (AA, BB and AB) follow a binomial distribution. Because of the different grains sizes of omphacite and garnet, the eclogites were evaluated using the surface model. It can be shown that their microstructures deviate from spatial random distributions showing various degrees of anticlustering and in many cases, the degree of anticlustering depends on direction, being stronger in the direction of the stretching lineation than in direction of the foliation normal. From this we infer that diffusion creep occurred by solution-precipitation processes and heterogeneous nucleation. A more general model for random distribution considers only one phase (A) and two types of grain contacts (AA and AB, where B is the "matrix"). This model is based on fragmenting a cluster of grains into smaller clusters. It predicts the most probable distribution of cluster sizes and the probability for contact types AA and AB. A comparison of the three models for random spatial distribution of grains shows that the discrimination of random from non-random patterns and the associated statistics depend strongly on the assumptions made concerning the nature of the underlying random process.
DE: 8030 Microstructures
DE: 8160 Rheology: general (1236, 8032)
SC: Mineral and Rock Physics [MR]
MN: 2007 Fall Meeting