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Geology; March 2009; v. 37; no. 3; p. 259-262; DOI: 10.1130/G25355A.1
© 2009 Geological Society of America
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Magmatic anhydrite-sulfide assemblages in the plumbing system of the Siberian Traps

Chusi Li1,*, Edward M. Ripley1, Anthony J. Naldrett2, Axel K. Schmitt3 and Craig H. Moore1

1Department of Geological Sciences, Indiana University, Bloomington, Indiana 47401, USA
2Department of Geology, University of Toronto, Ontario M5S 3B1, Canada
3Department of Earth and Space Sciences, University of California–Los Angeles, Los Angeles, California 90095, USA


Figure 01
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Figure 1. Kharaelakh intrusion, Siberia. A: Geological map. B: Cross section.

 

Figure 02
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Figure 2. Photomicrographs of magmatic anhydrite-sulfide assemblages in Kharaelakh intrusion.

 

Figure 03
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Figure 3. Relation between S content in basaltic melt at S saturation and oxidation state. FMQ—fayalite-magnetite-quartz.

 





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