Geochemistry of mercury mineralization and its environmental influence in the Tavreh area, west of Khoy, NW Iran

زمین شناسی اقتصادی

Article 4, Volume 3, Issue 2 - Serial Number 5, February 2012, Pages 183-192   

Document Type: Research Article

DOI: 10.22067/econg.v3i2.11446

Authors

Ali Imamalipour^* ; Jafar Abdollahei Sharif

Urmia

Abstract

Mercury mineralization has occurred in relation with a listwaenitic type hydrothermal alteration system in Tavreh area located northwest of Khoy. Mercury-bearing alteration zone which has an area about 0.4 km2 is situated in one of Aland river upstreams. The only mercury compound found in this district is mercury sulfide (cinnabar) deposited as vein and veinlet forms. Geochemical investigations indicate that mercury distribution has variable values which vary between 0.36-10500 ppm. Its average in alteration zone is 300 ppm, although its average reaches to 0.35 percent in the mineralized veins. Considering the Clarke amount of mercury, it has increased more than 3750 times in overall alteration zone and more than 46000 times in mineralized veins. Based on the stream sediment heavy mineral geochemistry, distribution of cinnabar under physical weathering and transportation processes has occurred at least 7 km far away from the altered zone in downstream sediments. Mercury concentrations in samples taken from surface and underground waters are less than 0.1µg/L. In comparison with mercury concentrations, data obtained from other world’s ore fields and considering the maximum permissible contaminant level in drinking waters, it can be concluded that the waters of this region have not been contaminated in mercury. Therefore, despite the extent of anomalous zone in Tavreh region, this zone cannot play a role as the contaminant source of environment. It is seemed that due to presence of mercury as stable mercury sulfide compound, the possibility of its leakage could not been obtained due to decomposition of this mineral.

Keywords

Khoy; Tavreh; listwaenite; mercury; Geochemistry; mineralization; Environment; contamination

References

[1] United states environment protection agency, 1997, Mercury study report to congress, vol.1.

[2] Laznicka P., "Emiricalmetallogeny", Elsevier scince pub1985.

[3] امامعلی پور ع.،"فلززایی جیوه در سنگهای لیستونیتی گستره افیولیتی خوی"، بیست و دومین گردهمایی علوم زمین، سازمان زمین شناسی کشور، تهران، بهمن ماه 82.

[4] امامعلی پور ع.، عبدالهی شریف ج.، حسنی پاک ع.، صحرایی ف.، "اکتشاف جیوه تیپ خان گلی چالدران"، شرکت مهندسین مشاور کاوشگران, 1382.

[5] امامعلی پور ع.، "بررسی ژئوشیمی کانی سازی جیوه و تأثیر زیست محیطی آن در منطقه طوره، باختر شهرستان خوی فلززایی ذخایر معدنی در گستره استان آذربایجان غربی"، طرح مصوب حوزه پژوهشی دانشگاه ارومیه,1390.

[6] MasonB., Moore C. B., "Principles of geochemistry", John Willey and sons 4th Ed1982.

[7] Horvat M., Jereb V., Logar M., Fajon V., Miklavcic V., "The impact of mercury mining on the environment and on human health in the wider"Idrija region, Slovenia 2002.

[8] Gemici U., Oyman T., "The influence of the abondanedKalecik Hg mine on water and stream sediments (Karaburun, Izmir, Turkey)", The science of the total environment, Elsevier 2003.

[9] http:// water-research.net (2010).

[10] مؤسسه استاندارد و تحقیقات صنعتی ایران، "ویژگیهای آب آشامیدنی"، استاندارد شماره 1053، چاپ چهارم1387.