Master of Science in Geoscience
First Committee Member
Eugene l. Smith, Chair.
Second Committee Member
Rodney V. Metcalf
Third Committee Member
Terry L. Spell
Graduate Faculty Representative
Number of Pages
Alkali basalts on Citadel Mountain form the southern margin of the Lunar Crater Volcanic Field (LCVF) in the central Great Basin, Nevada. Citadel Mountain comprised of a faulted, north tilted section of Tertiary andesite and ash-flow tuff is capped by Pliocene and Quaternary alkali basalt flows that erupted from six major cinder cones. The basalt flows on Citadel Mountain can be divided into two groups (older and younger) based on age and isotopic signatures. The older basalt group is characterized by higher 87 Sr/86Sr and lower ENd and the younger group has lower 87Sr/86Sr and higher ENd. Geochemical evidence suggests that the older basalt group is contaminated by a lithospheric mantle melt. A model is presented that shows contamination of the older alkali basalts by magma commingling/mixing of rising asthenospheric melts with lithospheric mantle veinlets in the mantle lithosphere. Fractional crystallization of olivine and clinopyroxene can explain the chemical variation in the older basalt group, and although small amounts of assimilation of upper crustal material are permissible, assimilation is not required in the models. The younger basalt group evolved solely by fractional crystallization of olivine and clinopyroxene and their isotopic signatures may reflect their asthenospheric mantle source.
Basalt—Composition; Geochemistry; Nevada; Radioactive dating; Strontium—Isotopes; United States--Great Basin
Geochemistry | Geology | Volcanology
University of Nevada, Las Vegas
Dickson, Loretta D., "Volcanology and Geochemistry of Pliocene and Quaternary Basalts on Citadel Mountain, Lunar Crater Volcanic Field, Pancake Range, Nevada" (1997). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1118.
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