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Investigating deep sea mineral deposits

 
INVESTIGATING DEEP SEA MINERAL DEPOSITS
NanoSIMS elemental maps of sulfide samples from the Mid-Atlantic Ridge show the remobilization and re-distribution of trace elements during the alteration of sulfides.
A) Irregular alteration of chalcopyrite.
B) Alteration of isocubanite along the margins.
C) Isocubanite enclosed in zoned sphalerite.
D-E) Different degrees of alteration of chalcopyrite.
F) Alteration of isocubanite.


Recorded on CAMECA NanoSIMS 50L at University of Western Australia. Image courtesy of P. Guagliardo (UWA) and Y. Wu (USJ, Macau).