Differentiation of the sulfides in the Basal Zone of the Stillwater Complex, Montana
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Abstract
Chemical leaching and analysis of the sulflde portion of rocks from a section of the Basal zone of the Stillwater Complex demonstrate that mole fractions of nickel, copper, cobalt, and sulfur in the sulfldes show trends and repeating patterns when plotted against stratigraphic position. These patterns are attributed to differentiation of immiscible sulflde liquids probably in response to differentiation of basaltic magma. Changes in composition of the immiscible sulflde liquids could most readily take place during the collection of the sulflde from the basaltic magma or during the crystallization of the sulflde liquid to the present assemblages of minerals.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Differentiation of the sulfides in the Basal Zone of the Stillwater Complex, Montana |
Series title | Journal of Research of the U.S. Geological Survey |
Volume | 6 |
Issue | 4 |
Year Published | 1978 |
Language | English |
Publisher | U.S. Geological Survey |
Description | 10 p. |
First page | 473 |
Last page | 482 |
Country | United States |
State | Montana |
Other Geospatial | Stillwater Complex |
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