The importance of supersaturated silica deposition for base-metalAu–Ag mineralisation in western Turkey
Author(s) -
Gülcan Bozkaya,
David Banks
Publication year - 2015
Publication title -
turkish journal of earth sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.356
H-Index - 43
eISSN - 1303-619X
pISSN - 1300-0985
DOI - 10.3906/yer-1405-10
Subject(s) - quartz , base metal , hydrothermal circulation , geology , flashing , supersaturation , deposition (geology) , mineralogy , metal , geochemistry , amorphous solid , metallurgy , materials science , chemistry , sediment , geomorphology , crystallography , organic chemistry , welding , seismology , paleontology
In the Arapucandere LS-IS epithermal deposit in western Turkey, either well crystallised euhedral quartz or milky amorphous silica occurrences are associated with the precious and base-metal mineralisation. This study has determined the relative importance of the processes precipitating both of these in relation to the deposition of the ore. Analysis by LA-ICPMS of euhedral quartz and amorphous silica show that the latter is associated with much higher metal concentrations and suggests that the process responsible is more important for deposition of ore in the deposit. Mineralisation at Kumarlar and Koru may be similar. Slow cooling precipitates euhedral quartz and some ore but flashing of hydrothermal fluids causes drastic decreases in both T and P, sufficient to quantitatively deposit base metals and Au. In amorphous silica bands base metals reach concentrations of 1000?s of ppm compared with a few 10?s ppm in euhedral quartz; Au can reach over 1 ppm compared with a few 10?s ppb in quartz. The drastic pressure change from lithostatic to sub-hydrostatic could reasonably be caused by opening of faults and fractures by seismic events.
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