Abstract
Devil's Gate limestone under cathodoluminescence. Bright yellow and orange areas are calcite and the bright blue indicates trace minerals along the solution seam. Trace minerals left in the seam are heavy metals and other silicate minerals.
Recommended Citation
Dvorak, Katherine
(2017)
"Stylolites Cathodoluminescence under Cross Polarized Light,"
The Hilltop Review: Vol. 10:
Iss.
1, Article 8.
Available at:
https://scholarworks.wmich.edu/hilltopreview/vol10/iss1/8
Included in
Geochemistry Commons, Geology Commons, Inorganic Chemistry Commons, Tectonics and Structure Commons
