Figure 13. (1) A
TIMS image (5-3-1 decorrelation stretch) and (2) corresponding
geologic map showing several important map units. Figure 14
shows the TIMS (red squares) and lab (blue diamonds) spectra for
six rock types from localities noted on the geologic map.
The TIMS imagery is partially successful at discriminating the
Proterozoic gneiss from the tonalite pluton, with differences
seen both in the image and in the spectral data. The gneiss
has a distinctive red-blue striped appearance in the northern
portions of this 5-3-1 image, where it consists of a relatively
thick sequence of banded amphibolite and quartzo-feldspathic
(Q-F) gneiss. The gabbroic and ultramafic rocks, (C) and
(D), are easily differentiated from the surrounding units but not
from each other.
Figure 14. Thermal
emission spectra for rocks found in the White Tank
Mountains. Red spectra represent spectra derived from the
six bands of the TIMS imager. Blue lines represent spectra
derived from a thermal spectrometer that have been deconvolved to
TIMS resolution.
Bedrock Geology Project
Abstract
Overview
Proterozoic rock units
Proterozoic Structures
Remote Sensing techniques
References and
Acknowledgments
Geology and Web pages by Steven Wood and Stephen J. Reynolds, Dept. of Geology, Arizona State University, Tempe, AZ -- July 1998