Publication Date
1996
Document Type
Dissertation/Thesis
First Advisor
Walker, Jim
Degree Name
M.S. (Master of Science)
Legacy Department
Department of Geology
LCSH
Geochemistry--Missouri; Geology--Missouri
Abstract
he Cope Hollow Formation (CHF) is the uppermost sequence of volcanic rocks exposed in the St. Francois Mountains (SFM). The formation consists mainly of >100 m of rhyolitic ash flow tuffs with interbedded basaltic lava flows. The CHF represents a marked change in the magmatism of the SFM, both chemically and mineralogically. The CHF rhyolites are higher in Na20, MgO, MnO, A1203, and Ti02 and lower in Si02 and K20, compared to underlying SFM rhyolites. The most notable mineralogic distinctions of the CHF rhyolites are their greater abundance of plagioclase phenocrysts and the lack of quartz phenocrysts, with the exception of the uppermost units. Within the CHF, four basaltic lava flows are present. These basalts and other basic rocks collected from several locations in the SFM help constrain the tectonic setting of the SFM which was dominated by acidic magmatism. There are essentially three groups of mafic rocks in the SFM, from oldest to youngest these are the SFM Andesite Suite, the Silvermines Mafic Suite and the Skrainka Mafic Suite, the latter two after Sylvester (1984). On AFM diagrams, all of these groups fall in the tholeiitic field. Incompatible element ratios of all three groups (NB/La, Hf/Ta, La/Ta, Ti/Y, Hf/Th, Th/Yb, Th/Nb, Zr/Y, and Ta/Yb) consistently show arc affinities. The ratios Zr/Y and Ta/Yb are greater than 3 and 0.1 respectively, suggesting an overall continental margin affinity. There are, however, some distinctions in incompatible element ratios among the 3 mafic suites, suggesting that the magmatic source, and perhaps some aspect of the tectonic setting, changed with time. For example, Zr/Nb ratios differ by a factor of three between the Silvermines and Skrainka groups, suggesting a shift towards a more depleted source for the younger Skrainka suite.
Recommended Citation
Pippin, Charles G., "Geology and geochemistry of the Cope Hollow Formation and the Western St. Francois Mountains, southeastern Missouri" (1996). Graduate Research Theses & Dissertations. 3276.
https://huskiecommons.lib.niu.edu/allgraduate-thesesdissertations/3276
Extent
xi, 182 pages
Language
eng
Publisher
Northern Illinois University
Rights Statement
In Copyright
Rights Statement 2
NIU theses are protected by copyright. They may be viewed from Huskie Commons for any purpose, but reproduction or distribution in any format is prohibited without the written permission of the authors.
Media Type
Text
Comments
Includes bibliographical references (pages [155]-164)