@conference{
author = "Krstić, Nenad S. and Pavlović, Mirjana S. and Nikolić, Nebojša D. and Đorđević, Miloš G. and Premović, Pavle I.",
year = "2010",
abstract = "Geochemical analyses for trace Cr have been made on a representative sample of a
typical hydrothermal dickite filling vein at Nowa Ruda. The mineralogy of the
sample is comparatively simple, dickite being the principal component (ca. 91% of
total sample). Geochemical fractionation and inductively coupled plasma-optical
emission spectrometry (ICP-OES) indicate that most (>96 % of total metal) of Cr
reside in the dickite. The combination of geochemical and spectroscopic tools
applied on Cr3+ allow one to specify the Eh (>0.4 V, highly oxidizing) and pH
(≤4.0, highly acidic) of the solution during the formation of dickite from the Nowa
Ruda Basin. We suggest that hot hydrothermal waters leached the surrounding
varieties of gabbroids enriched in Cr for the dickite-forming solution.",
publisher = "Society of Physical Chemists of Serbia",
journal = "Physical chemistry 2010 : 10th international conference on fundamental and applied aspects of physical chemistry",
title = "Geochemistry of the hydrothermal dickite (nowa ruda, lower silesia, poland): chromium",
url = "https://hdl.handle.net/21.15107/rcub_vinar_9346"
}