Abstract
dc:description.abstract<p>It was found, by determining the types of minerals found in the Harvey Lake area, that the sedimentary rocks of sandstone, dolostone, limestone, and shales were regionally metamorphosed to a degree of metamorphism corresponding with that of the “Staurolite-Almandine Subfacies” of the “Almandine-Amphibolite Facies.” These minerals were determined by hand-sample inspection, by thin-section observations, and by observing powdered samples immersed in refractive oils. </p>
Degree
thesis:*- Name thesis:degree_name
- Bachelor of Science (BS)
- Level thesis:degree_level
- Thesis
- Discipline thesis:degree_discipline
- Geology
- Year
- 1961
Author and committee
dc:creator, dc:contributor.*- Author dc:creator
-
- Davidson, Jerry
Identifiers
dc:identifier.*- Repository record dc:identifier
- https://commons.und.edu/senior-projects/119
- OAI identifier oai:identifier
- oai:commons.und.edu:senior-projects-1118