Temat: ore zone - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Delineation of ore zones using the concentration-volume fractal method in the Dagh Dali Zn-Pb (±Au) prospect, north of Takab (Iran)
Autorzy:: Motlagh, Zahra Yekani
Imamalipour, Ali
Bazdar, Habibollah
Powiązania:: https://bibliotekanauki.pl/articles/2059665.pdf
Data publikacji:: 2020
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: ore zone
concentration-volume
C-V
fractal method
kriging
micromine software
Dagh Dali
Opis:: The Dagh Dali Zn-Pb (±Au) hydrothermal prospect is located in the north-west of Iran. Identification of mineralized zones is essential in ore deposit exploration. Different methods have been developed and applied to separate mineralized zones from barren host rocks based on mineralogical and petrographical studies, alteration and host rock changes as well as statistical and geostatistical parameters. This study uses the ordinary kriging technique and the concentration-volume fractal (C-V) method to model the ore body and recognize the ore grade distribution. These techniques were applied on the drillcore data and C-V fractal modelling, values of various ore zones being determined. Four breakpoints were found in the log-log plots which correspond to concentrations of 5.4, 10.5, and 17.8 wt.% Zn. The extractable ore zone for Zn is considered to be in the concentaration range of 5.4 to 17.8 wt.%. Compared to the amount of reserve obtained from the geostatistical method (303,685 tons), it seems that the fractal method is more precise and accurate in the estimation of ore reserves.
Źródło:: Geological Quarterly; 2020, 64, 2; 275--287
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Determination of the nip zone angle in high-pressure grinding rolls
Autorzy:: Saramak, D.
Naziemiec, Z.
Powiązania:: https://bibliotekanauki.pl/articles/109355.pdf
Data publikacji:: 2013
Wydawca:: Politechnika Wrocławska. Oficyna Wydawnicza Politechniki Wrocławskiej
Tematy:: HPGR
comminution
nip zone
ore processing
Opis:: A proposal of the nip zone angle determination in high-pressure grinding rolls (HPGR) crush-ing process is presented in the paper. Knowledge of the nip zone angle value makes it possible to deter-mine the real maximum pressing force in the high-pressure comminution. Two methods of determination of this maximum pressure were proposed and verified. The first method is based on the roll’s geometry and the change of the HPGR chamber’s volume together with the roll rotation, while the second one considers the outlet gap width. Results of the nip zone angle calculations according to both methods are similar and show that the nip zone angle is around 3o. The verification was carried out in a piston-die press and experimental results show that the product size distributions from HPGR and piston-die press are similar. The methodology of the nip zone angle determination presented in the paper has then its practical confirmation. A proper determination of the nip zone border makes it possible to calculate the comminution probability of given type of material and is a basis for the HPGR crushing process modeling and optimization.
Źródło:: Physicochemical Problems of Mineral Processing; 2013, 49, 1; 243-253
1643-1049
2084-4735
Pojawia się w:: Physicochemical Problems of Mineral Processing
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: The Rietveld refinement studies of pyromorphite-vanadinite and mimetite-vanadinite solid solution series
Autorzy:: Solecka, U.
Zelek, S.
Bajda, T.
Powiązania:: https://bibliotekanauki.pl/articles/184341.pdf
Data publikacji:: 2016
Wydawca:: Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:: apatite supergroup
oxidation zone
ore deposit
Opis:: Mimetite Pb 5 (PO 4 ) 3 Cl, vanadinite Pb 5 (VO 4 ) 3 Cl and pyromorphite Pb 5 (PO 4 ) 3 Cl belong to the apatite supergroup. They form in oxidation zones of lead ore deposits. These minerals have high thermal stability (Dong et al. 2002) and low solubility (Flis et al. 2011) thus they have many applications. Pyromorphite and mimetite are especially used to immobilize lead in contaminated soils and hazardous industrial wastes (Ma et al. 1993, Kim et al. 2005, Bajda et al. 2007), it is therefore important to know the impact of various factors on their properties. Crystal structure of apatites corresponds to the general formula M 5 (TO 4 ) 3 X, where M are bi - valent cations distributed on two distinct crystallographic sites, TO 4 is a trivalent oxyanion and X is a monovalent anion. The structure and chemistry of apatite allow for numerous substitutions of metal cation and anionic complexes (Hughes & Rakovan 2002, Pan & Fleet 2002). It was found that substitutions cause variations in the unit cell parameters and chemical properties of these minerals (Botto et al. 1997), but there are no articles presenting variations in the whole series. Therefore, these researches present changes of lattice parameters for pyromorphite-vanadinite and mimetite-vanadinite solid solution series. Pyromorphite, mimetite and vanadinite crystallize in hexagonal symmetry (the space group P6 3 /m) (Dong et al. 2002, Pan & Fleet 2002). They form continuous isomorphic series. The aim of study was to examine how lattice parameters of pyromorphite-vanadinite and mimetite-vanadinite solid solutions series change with increasing vanadium content and characterize these pheno mena. Crystallographic studies were conducted on synthetic pyromorphite, mimetite and vanadinite and minerals with intermediate compositions Pb 5 (TO 4 ) 3 Cl, where T = P + V or As + V, of various P/V or As/V ratios. Samples were analyzed by X-Ray diffraction (XRD) using RIGAKU Smartlab X-Ray diffractometer with Cu radiation in a 10° to 110° 2Θ range at a step size of 0.02 2Θ and a rate of 2 s per step. The phase identification was carried out using the X’Rayan computer program and X-ray standard patterns in the form of ICDD files (card 19-0701, 19-0683 and 43-1461). The unit-cell refinement and Rietveld structure refinement were made using the FullProf Suite computer program package (Rodriguez-Carvajal 1993). The Rietveld refinement has shown systematic changes in unit cell parameters of studied samples depending on their chemical composition. Dimensions of unit cell parameters of pyromorphite-vanadinite solid solution series increase linearly with the substitution of vanadate ions in the structure of pyromorphite. Lattice parameter “a” increase in the range of 9.987–10.325 Å, while lattice parameter “c” increase in the range of 7.33–7.343 Å. In case of the mimetite-vanadinite solid solution series, lattice parameter “a” increase (10.251–10.325 Å range), whereas lattice parameter “c” decrease (7.442–7.343 Å range) linearly with the substitution of vanadate ions in the structure of mimetite. This situation indicates the equivalent position of the tetrahedral TO 4 in the structure of lead apatite.
Źródło:: Geology, Geophysics and Environment; 2016, 42, 1; 127-128
2299-8004
2353-0790
Pojawia się w:: Geology, Geophysics and Environment
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Zmienność mineralizacji kruszcowej w spągowych utworach cechsztynu na granicy strefy utlenionej i redukcyjnej w zachodniej części złoża Polkowice
Variability of ore mineralization in the lowermost Zechstein across the redox interface in the western part of the Polkowice deposit
Autorzy:: Chmielewski, A.
Powiązania:: https://bibliotekanauki.pl/articles/2063047.pdf
Data publikacji:: 2011
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: mineralizacja kruszcowa
strefa utleniona
strefa przejściowa
strefa redukcyjna
łupek miedzionośny
cechsztyn
ore mineralization
Rote Fäule
transition zone
reducing zone
Kupferschiefer
Zechstein
Opis:: Przedmiotem niniejszej pracy jest zmienność mineralizacji kruszcowej na granicy strefy utlenionej i redukcyjnej w profilach cechsztyńskiej serii miedzionośnej z archiwalnych otworów wiertniczych, usytuowanych w zachodniej części złoża Polkowice, w najbliższym sąsiedztwie bloku przedsudeckiego. Zidentyfikowano następujące minerały kruszcowe: chalkozyn, kowelin, digenit, tennantyt, bornit, chalkopiryt, kobaltyn, skuterudyt, nikielin, rammelsbergit, piryt, galenę, sfaleryt i markasyt. Określono budowę wewnętrzną skał złożowych, relacje pomiędzy składnikami skał oraz opisano litologię tych utworów. Zmienność mineralizacji kruszcowej w profilach wiertniczych serii złożowej wskazuje na występowanie bogatej mineralizacji miedziowej ponad utworami utlenionymi (głównie w formie rozproszonej) oraz obecność złota w utworach utlenionych (złoto submikroskopowe).
A full-scale investigation into variability of ore mineralization at the contact between oxidized and reduced zone in the copper-bearing Zechstein series was performed. Results of the studies were obtained on the basis of archival boreholes located in the western part of the Polkowice mining area, proximal to the Fore-Sudetic Block. Detailed microscopic observations enabled to identify the following ore minerals: chalcocite, covellite, digenite, tennantite, bornite, chalcopyrite, cobaltite, skutterudite, nickeline, rammelsbergite, pyrite, galena, sphalerite and marcasite. Microscopic observations allowed determining some features of host sediments (textures and structures) and establishing relations between constituents of rocks. Petrographic analysis of thin-sections also allowed describing the lithology of the rocks. The variability of ore mineralization in the boreholes indicates the occurrence of high-grade copper ores (mainly disseminated mineralization) above the oxidized zones, and the presence of submicroscopic gold in oxidized rocks.
Źródło:: Biuletyn Państwowego Instytutu Geologicznego; 2011, 444; 33--53
0867-6143
Pojawia się w:: Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:: Biblioteka Nauki

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