TY  - CONF
AU  - Krstić, Nenad S.
AU  - Pavlović, Mirjana S.
AU  - Nikolić, Nebojša D.
AU  - Đorđević, Miloš G.
AU  - Premović, Pavle I.
PY  - 2010
UR  - https://vinar.vin.bg.ac.rs/handle/123456789/9346
AB  - 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.
PB  - Society of Physical Chemists of Serbia
C3  - Physical chemistry 2010 : 10th international conference on fundamental and applied aspects of physical chemistry
T1  - Geochemistry of the hydrothermal dickite (nowa ruda, lower silesia, poland): chromium
UR  - https://hdl.handle.net/21.15107/rcub_vinar_9346
ER  - 

@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"
}

Krstić, N. S., Pavlović, M. S., Nikolić, N. D., Đorđević, M. G.,& Premović, P. I.. (2010). Geochemistry of the hydrothermal dickite (nowa ruda, lower silesia, poland): chromium. in Physical chemistry 2010 : 10th international conference on fundamental and applied aspects of physical chemistry
Society of Physical Chemists of Serbia..
https://hdl.handle.net/21.15107/rcub_vinar_9346

Krstić NS, Pavlović MS, Nikolić ND, Đorđević MG, Premović PI. Geochemistry of the hydrothermal dickite (nowa ruda, lower silesia, poland): chromium. in Physical chemistry 2010 : 10th international conference on fundamental and applied aspects of physical chemistry. 2010;.
https://hdl.handle.net/21.15107/rcub_vinar_9346 .

Krstić, Nenad S., Pavlović, Mirjana S., Nikolić, Nebojša D., Đorđević, Miloš G., Premović, Pavle I., "Geochemistry of the hydrothermal dickite (nowa ruda, lower silesia, poland): chromium" in Physical chemistry 2010 : 10th international conference on fundamental and applied aspects of physical chemistry (2010),
https://hdl.handle.net/21.15107/rcub_vinar_9346 .