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Finally, Electron BackScattered Diffraction (EBSD) maps are collected for specimens with large grains and small defects.
After the processing described in Sections 1.3.1 to 1.3.3, Gabor and PC maps are collected for a specific image, which are relevant on the fine level.
At the final stage, the resulting individual spatial component maps are collected across subjects into single 4D files (1 per original ICA network map, with the fourth dimension being subject to identification).
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Maps were collected using high field blood oxygenation level dependent (BOLD) functional magnetic resonance imaging (fMRI).
Historical soil survey reports and soil maps were collected, scanned, and summarized.
MA-XRF maps were collected using a Bruker M6 Jetstream Instrument from Bruker [25].
Macroscopic X-ray fluorescence maps were collected using a Bruker M6 Jetstream instrument [14].
The strain maps were collected from several types of Nd2Fe14B grains in contact with metallic-Nd (m-Nd), Nd2O3, NdOx, and thin grain boundary phases.
Residual gravity maps were collected over various spatially distributed ore bodies for determining approximately the quantity of chromite in any deposits found.
Two-dimensional Raman maps were collected in a few cases to show distributions of exsolved amphibole with other exsolved phases in garnet.
Ultrasound images and associated elastographic maps were collected at 0, 2 and 3 kPa in the intact state and strains on the internal surface were calculated using stereo-correlation in all states.
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