South-Central Section - 51st Annual Meeting - 2017

Paper No. 5-2
Presentation Time: 9:00 AM-5:30 PM

MODAL MINERALOGICAL ANALYSIS OF ROCKS IN THIN SECTION USING STATISTICAL ANALYSIS OF X-RAY MAPS IN ARCGIS


URBANCZYK, Kevin M. and BAILEY, William, Department of Biological, Geological and Physical Sciences, Sul Ross State University, Box C-139, Alpine, TX 79832, wlb14wj@sulross.edu

We have conducted modal analysis of thin sections of the Luna Vista sill using classification routines in ArcGIS. The technique is similar to other classification schemes (e.g. a supervised multispectral classification of Landsat data), but uses X-ray maps generated with an Energy Dispersive X-ray detector instead of spectral “bands” of electromagnetic radiation. We are using a specific adaptation of this ArcMap capability created by Ortolano and others (2014).

The Luna Vista Sill (LVS) is located in the Christmas Mountains in southern Brewster County. The LVS has a peralkaline quartz trachyte composition. The mineralogy of the rock includes alkali feldspar, arfvedsonite, eckermannite, ferro-eckermannite, aegirine augite, apatite with rare earth elements (REEs), zircon, ilmenite, hematite, calcite, and quartz. X-ray maps of thin sections of the LVS have been created for the elements Si, Ti, Al, Fe, Mg, Mn, Ca, Na, and K using an Energy Dispersive detector on a JEOL 6010LA SEM at the Sul Ross State University Analytical Laboratory. The X-ray maps are raster images in tiff format that include an 8-bit (0-255) signal per pixel for each element. The technique includes the initial application of a "Low Pass" or a "Focal Median" filter to reduce potential instrument noise, followed by a Principle Component Analysis (PCA). This technique exploits the natural variation in the multiband data by creating a new multivariate space and a new multiband raster with the same number of principle components as were in the original X-ray map set. This is followed by an unsupervised or a supervised classification to determine the mineral "classes" that exist in the thin section. The results can be used to estimate the modal mineralogical abundance in the rocks.