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Fabric Analyser

A computer-controlled macroscope (G50) has rotating polarising filters above and below the stage. The LED illumination system is polyaxial with a vertical axis and eight inclined axes. The high resolution four megapixel camera transfers images to the controlling notebook computer at 15 frames per second via Gigabit Ethernet.

This provides an automated data acquisition system that can be used for the collection of c-axis crystallographic fabric data in hexagonal mineral systems in rocks, ice aggregates and in apatite fission track mounts. This instrument can be purchased by contacting Chris Wilson (cjlw@unimelb.edu.au).

G50diagram
G50 set-up for collection of microstructural data.

The stage can accommodate thin sections of up to 100 x 100 mm with motors controlling translations in the X and Y directions to 5 µm resolution. No tilting of the thin section is required for the analysis. The software system on the computer controls the stage and captures images directly from the camera. Composite optical images of the total thin section are then used for the analysis of the c-axis at any particular point or over a selected area (enabling whole thin section analysis).

The analysis process works in two stages:

  1. The analytical instrument scans the thin section and collects and processes image data.

  2. The section data acquired from the analytical instrument is loaded into a separate analysis software (called INVESTIGATOR) that allows the operator to examine individual crystallographic variation across individual grains. Unlike traditional texture analysis the information allows considerable interactive data processing, using INVESTIGATOR, as the link between microstructure and individual c-axis orientations.

Left Hand Side NavigationTo interactive grain selection

flow

Multiple images can be generated such as AVA (orintation distribution maps), geometric quality and retardation maps. The geometric quality map represents c-axis colatitudes (angle from the vertical) versus their geometric qualities. The retardation maps visualise c-axis azimuths and their related retardation quality.The data set can also be used to obtain distribution of crystal outlines, location of inclusions and ascertain nearest neighbour grain relationships.

Photo of an analyser
A version of apparatus for fine grained rocks (MiFA). See description in Wilson et al. 2007 (Journal of Microscopy).

 
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