T191 Mineralogical Evidence for the Co-Evolution of the Geosphere and Biosphere: In Honor of Robert M. Hazen, 2016 Roebling Medalist
Tuesday, 27 September 2016
8:00 AM - 12:00 PM
Room 207
SOCIAL NETWORK OF COPPER MINERALS: A MINERAL ECOLOGY STUDY
Paper number: T191-7
Program: Technical Sessions
Time: 9:40 AM – 9:55 AM
Authors
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Daniel R. HummerCarnegie Institution of Science, Washington, DC, DC
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Chao LiuCarnegie Institution of Science, Washington, DC, DC
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Michael MeyerCarnegie Institution of Science, Washington, DC, DC
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Jolyon RalphSurrey
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Grethe HystadPurdue University Northwest, Hammond, IN
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Robert HazenCarnegie Institution for Science, Washington, DC
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Robert T. DownsUniversity of Arizona, Tucson, AZ
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Joshua J. GoldenUniversity of Arizona, Tucson, AZ
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Alexander J. PiresUniversity of Arizona, Tucson, AZ
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Peter FoxRensselaer Polytechnic Institute, Troy, NY
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Xiaogang MaRensselaer Polytechnic Institute, Troy, NY
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Stephan ZednikRensselaer Polytechnic Institute, Troy, NY
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Ahmed EleishRensselaer Polytechnic Institute, Troy, NY
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Sophia KolankowskiRensselaer Polytechnic Institute, Troy, NY
Abstract
As expected, common minerals form nodes around which less common minerals cluster. Cu minerals also tend to form distinct groups as a function of anion or anion complex, particularly around sulfides, sulfates and oxides. Furthermore, Cu minerals cluster according to rock and deposit type, such as hydrothermal sulfide veins and fumarole deposits, illustrating the geologic connectivity of mineral co-occurrence.
Cochran-Mantel-Haenszel statistical analyses of 3-element mineral correlation demonstrate chemical and geologic trends in the Cu system. With this method, we found that the presence of Cu enhances the relationship between oxygen and other chalcophile elements. We also observed that Cu-sulfates are less abundant than expected and Cu-silicates are slightly more abundant than expected based on first-order mineral composition trends.
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-279379
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