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2 2009

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Additional exploratory boreholes optimization based on three-dimensional model of ore deposit

Soltani S., Hezarkhani A.

Archives of Mining Sciences

2009

Vol. 54, no 3

495-506

Contrary to other methods employed in optimization of the location of additional boreholes drilling, in this article, three-dimensional development of ore deposits and boreholes are attended for calculation of objective function (maximization of "estimation variance reduction") as well as for seeking optimum pattern of additional boreholes. This method leads to increase of estimation variance calculation accuracy as well as more efficient boreholes positioning. Moreover, in this development, it is possible to integrate initial directional boreholes in the studies of additional boreholes optimization. In this article, the method employed for finding the location of additional exploratory boreholes of Iju Porphyry copper deposit is used as a case study, and the results are referred. The results indicate that having considered three-dimensional development of ore deposits and boreholes in homogeny massive shape ore deposits has increased efficiency of the proposed pattern.

W odróżnieniu od metod wykorzystywanych w optymalizacji rozmieszczenia dodatkowych otworów badawczych, trójwymiarowe obrazowania złóż rudy oraz samych otworów wykorzystywane są do obliczania funkcji celu (wyrażonej jako maksymalizacja redukcji estymacji wariancji) oraz do poszukiwania optymalnych układów prowadzenia dodatkowych otworów. Metoda ta pozwala na zwiększenie dokładności obliczenia estymacji wariancji i co za tym idzie, poprawia efektywność lokalizacji otworów. Ponadto, w podejściu tym możliwe jest zintegrowanie wstępnych położeń otworów dla celów optymalizacji. Artykuł ten przedstawia studium przypadku czyli zastosowanie powyższej metody do lokalizacji dodatkowych otworów eksploracyjnych w złożu rud miedzi w Iju Porphyry wraz z omówieniem wyników. Wyniki wskazują, że rozpatrywanie trójwymiarowego modelu złoża rudy oraz otworów w jednolitym górotworze pozwala na zwieszenie efektywności proponowanego rozwiązania.

The comparison of alteration zones in the Sungun porphyry copper deposit, Iran (based on fluid inclusion studies)

Asghari O., Hezarkhani A., Soltani F.

Acta Geologica Polonica

2009

Vol. 59, no. 1

93-109

The Sungun porphyry copper deposit (PCD) is located in East Azarbaijan, in northwestern Iran. The felsic rocks occur as stocks and dykes ranging in composition from quartz monzodiorite through quartz monzonite. The stocks are classified into porphyry stocks I and II. Porphyry stock II, hosting the copper ore, experienced an intense hydro-fracturing leading to the formation of stockwork-type veinlets and micro-veinlets of quartz, sulphides, carbonates and sulphates. Three distinct types of hydrothermal alteration and sulphide mineralization are recognized at Sungun (1) hypogene, (2) contact metasomatic (skarn), and (3) supergene. Hypogene alteration is developed in four kinds: potassic, phyllic, propylitic and argillic. Three types of fluid inclusions are typically observed at Sungun: (1) vapour-rich, two-phase, (2) liquid-rich two-phase and (3)multi-phase. Halite is the principal solid phase in multiphase inclusions. Primary multiphase inclusions (LVH type fluid inclusions) within the quartz crystals in quartz-sulphide and quartz-molybdenite veinlets (quartz associated with sulphide minerals) were selected for micro-thermometric analyses and considered to be suitable for pressure calculations and estimation of hydrothermal fluid density. Homogenization temperature, salinity, pressure and density were measured and calculated in forty-seven selected samples. None of the variables could distinguish the potassic from phyllic alteration zones clearly. In the potassic alteration zone, the average of homogenization temperature is about 413[degrees]C, while in the phyllic alteration zone its average is about 375[degrees]C. It was expected that the temperature in the potassic alteration zone would be higher than that in the phyllic zone, but the difference found was not very significant The fluid inclusion salinity within both alteration zones obviously relates to their homogenization temperature: the average salinity in the samples from the potassic zone is 46.3 (wt%NaCl equiv.), which is higher than that in the samples from the phyllic zone. Based on the estimated depth of the potassic alteration domain, it is expected that the lithostatic pressure was higher than in the phyllic alteration zone. According to the fluid inclusion studies and pressure calculation, it is estimated that the average pressure for the potassic alteration zone was about 512 (bars) while the average pressure for phyllic zone was about 310 (bars). The average density of fluids in the samples from the potassic alteration zone is 1.124 (g/cm[^3]), which is higher than that in the phyllic alteration zone (1.083 g/cm[^3]).