Clicking on the images will display larger versions of the photos.
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SEM image (3,000x) of limestone grains. Individual calcite grains are
approximately 2.5 microns with smooth intergrown blocks with no pits.
Samples are Au-Pd coated. Photomicrograph by Spilde.
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EDS spectrum of previous image of limestone grains, showing that the
limestone is pure calcite. Samples are Au-Pd coated. Analysis by Spilde.
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EDS spectrum of large crystal in the inner wall rock at EY56 in the Western
Borehole. EDS suggests the crystal is calcite. EDS of several locations
within the inner wall rock at this location showed the same composition
whether they were defined crystals or not. Some had a little more
magnesium. Samples are Au-Pd coated. Analysis by Spilde, Northup, and Boston.
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EDS spectrum of inner wall rock from EY56 in the Western Borehole. Notice
the presence of sulfur, potassium, and iron peaks in addition to the clay
elements. Samples are Au-Pd coated. Analysis by Spilde, Northup, and Boston.
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EDS spectrum of bright particles in outer wall rock sample from EY56 site in the
Western Borehole. Peaks include iron, vanadium, oxygen, silicon, and
aluminum. Samples are Au-Pd coated. Analysis by Spilde, Northup, and Boston.
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SEM image of dolomite in the outer wall rock sample from EY56 site in the
Western Borehole. Photo by Spilde, Northup, and Boston.
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SEM image of a putative apatite crystal in the outer wall rock sample from
EY56 in the Western Borehole. Photo by Spilde, Northup, and Boston.
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EDS spectrum of bright particles in outer wall rock sample from EY56 site in the
Western Borehole. Peaks suggest the presence of apatite. Samples are
Au-Pd coated. Analysis by Spilde, Northup, and Boston.
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EDS spectrum of the area between the larger dolomite crystals in the outer
wall rock sample from EY56 site in the Western Borehole. A strong iron
signal is observed. Not shown, but detected in the surrounding areas are
barite crystals and gypsum particles. Samples are Au-Pd coated. Analysis
by Spilde, Northup, and Boston.
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EDS spectrum of bright crystals the outer
wall rock sample from EY56 site in the Western Borehole. A strong iron
signal is observed. Samples are Au-Pd coated. Analysis
by Spilde, Northup, and Boston.
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