Masters Theses
Abstract
"The Boss-Bixby deposit is located on the line dividing Iron and Dent Counties and belongs to the Southeast Missouri Precambrian Iron Metallogenic Province. The sequence of events leading to the formation of the deposit is reviewed. The mineralization occurred after intrusion of intermediate magma, but prior to the intrusion of granite. The ore minerals present are the following in the order of deposition: magnetite, ilmenite, giekielite, hematite, rutile, pyrite, molybdenite, cobaltite, chalcopyrite, bornite, sphalerite, galena, limonite, chalcocite, and cuprite. Four different methods of zoning are presented. Partial pressures of oxygen and sulphur [sic], as well as temperature controlled sequential deposition of ore. This deposit is classified as a pyrometasomatic body"--Abstract, page ii.
Advisor(s)
Kisvarsanyi, Geza
Committee Member(s)
Bolter, Ernst
Legsdin, Adolph, 1899-1969
Department(s)
Geosciences and Geological and Petroleum Engineering
Degree Name
M.S. in Geology
Publisher
University of Missouri--Rolla
Publication Date
1968
Pagination
vii, 94 pages
Note about bibliography
Includes bibliographical references.
Geographic Coverage
Missouri
Dent County (Mo.)
Boss County (Mo.)
Rights
© 1968 Frederick J. Smith, All rights reserved.
Document Type
Thesis - Open Access
File Type
text
Language
English
Subject Headings
Metallogeny -- MissouriMinerals -- Missouri -- Boss CountyMinerals -- Missouri -- Dent CountyMines and mineral resources -- Missouri
Thesis Number
T 2134
Print OCLC #
5998270
Electronic OCLC #
794121371
Recommended Citation
Smith, Frederick Joseph, "Mineralization of the Boss Bixby anomaly, Iron and Dent Counties, Missouri" (1968). Masters Theses. 5181.
https://scholarsmine.mst.edu/masters_theses/5181