Abstract/Details

Differentiation in the early Earth: An experimental investigation


1994 1994

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Abstract (summary)

The Earth may have been covered with a terrestrial magma ocean. Is there evidence for resulting extensive mineral fractionation? Agee and Walker, 1988, proposed that significant flotation and addition of olivine into the upper mantle can explain the elevated Mg/Si ratio of this region. A number of element ratios were present in the primitive mantle of the Earth in approximately chondritic ratios (e.g., Jagoutz et al., 1979) providing constraints on amounts of mineral fractionation if appropriate partition coefficient values are known (e.g., Kato et al., 1988a). In addition, the V, Cr and Mn abundance pattern in the mantles of the Earth and moon are similar to one another, which could imply a related origin for these bodies (e.g., Ringwood, 1990). Previous attempts to explain the origin of this abundance pattern have been unsuccessful (e.g., Drake et al., 1989).

High pressure and temperature mantle mineral/silicate melt partition coefficient values are experimentally determined in this work. These values are used via equilibrium crystallization to examine the effect of mineral fractionation on the primitive mantle. The effect of mineral fractionation on the abundance pattern of V, Cr and Mn in the upper mantle of the Earth is examined. Fractionation of majorite garnet, magnesiowustite and Mg-perovskite yields a V, Cr and Mn abundance pattern that is different than inferred. Thus, the pattern of V, Cr and Mn was not established by high pressure mantle mineral/silicate melt fractionation.

Other mineral fractionation effects are also examined. Significant addition of olivine to the upper mantle is disallowed based on the Ni/Co ratio. Significant fractionation of majorite garnet, magnesiowustite and Mg-perovskite is precluded based on several element ratios (e.g., Mg/Al, Ca/Al for majorite garnet; e.g., Mg/Al, Ca/Al, Mg/Si, Mg/Ca for magnesiowustite; e.g., Ca/Al, Sc/Sm, Mg/Ca for Mg-perovskite). Thus, the primitive mantle does not show evidence of significant fractionation of volumetrically important liquidus phases. The implication is that the Earth's Mg/Si ratio unique, and that compositionally distinct reservoirs of material were largely preserved in the accretionary environment.

Indexing (details)


Subject
Geochemistry;
Geology;
Mineralogy
Classification
0996: Geochemistry
0372: Geology
0411: Mineralogy
Identifier / keyword
Earth sciences; chromium; manganese; vanadium
Title
Differentiation in the early Earth: An experimental investigation
Author
McFarlane, Elisabeth Ann
Number of pages
153
Publication year
1994
Degree date
1994
School code
0009
Source
DAI-B 55/04, Dissertation Abstracts International
Place of publication
Ann Arbor
Country of publication
United States
Advisor
Drake, Michael J.
University/institution
The University of Arizona
University location
United States -- Arizona
Degree
Ph.D.
Source type
Dissertations & Theses
Language
English
Document type
Dissertation/Thesis
Dissertation/thesis number
9424944
ProQuest document ID
304118753
Copyright
Database copyright ProQuest LLC; ProQuest does not claim copyright in the individual underlying works.
Document URL
http://search.proquest.com/docview/304118753
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