Acta Mineralogica-Petrographica, Abstract Series 5, Szeged, 2006MORDENITE <strong>IN</strong> OPHIOLITES FROM <strong>THE</strong> METALIFERI MTS., ROMANIAKRISTÁLY, F. & SZAKÁLL, S.Department of Mineralogy and Petrology, University of Miskolc, H-3515 Miskolc-Egyetemváros, HungaryE-mail: askkf@gold.uni-miskolc.huMordenite is a common zeolite, with sedimentary (bydiagenesis in volcanic tuffs) or hydrothermal origin. Mordeniteis usually found in radial aggregates of acicular orfibrous crystals. Mordenite of hydrothermal origin is a frequentmember in hydrothermal mineral assemblages ofophiolites, or ocean-floor type metamorphosed rocks.Today’s known fibrous zeolites of the Metaliferi Mts. arenatrolite (?) (SZAKÁLL, 2002) and mesolite (BEDELEAN,1971; SZAKÁLL, 2002); mordenite has not been mentionedto date. The two studied occurrences of mordenite in theophiolite type rocks of Metaliferi Mts are at Săliştioara (anabandoned basalt quarry, sample S1) and in the Bodii valleyat Techereu (TB1 sample).At Săliştioara mordenite appears as fine fibrous aggregatesfilling amygdales of the altered basalt, up to 5 mm indiameter. The amygdales are white to pale rose and reddish,due to the hematite inclusions that are usually associated withreddish clinoptilolite.At Techereu mordenite appears as white, fibrous aggregates.The aggregates are nested in the calcite veins filling inthe voids between heulandite crystals. In contrast with theSăliştioara occurrence, in this case the colour of mordenitedoes not vary, but heulandite crystals show a white to reddishcolour zoning.The presence of mordenite was confirmed by X-ray powderdiffraction (Table 1).Five chemical analyses (Table 2) were carried out withEPMA (by Giovanna Vezzalini, at the University of Modena,Italy). H 2 O could not be determined due to the paucity ofavailable material. The results are similar to those publishedby PASSAGLIA (1975). The analyzed samples are Ca-Nadominant, with a low content of K and light variation of exchangeablecations.Samples of the investigated mordenite are deposited inthe mineral collection of the Herman Ottó Museum (Miskolc,Hungary).ReferencesBEDELEAN, I. (1971): Zeoliţii din Munţii Apuseni. Doctoraltheses, Manuscript. Babeş–Bolyai University, Cluj-Napoca.PASSAGLIA, E. (1975): Contributions to Mineralogy andPetrology, 50, 65–70.SZAKÁLL, S. (ed., with the contributions of UDUBAŞA,G., ĎUĎA, R., SZAKÁLL, S., KVASNYTSYA, V.,KOSZOWSKA, E. & NOVÁK, M.) (2002): Minerals ofthe Carpathians. Prague: Granit.Table 1: Strongest reflections of mordenite observed on the XRPD pattern of the samples.TB1 S1 ICDD 29-1257d (Å) I (%) d (Å) I (%) d (Å) I (%) hkl8.809 23.9 8.924 100 9.060 100 2003.968 2.8 3.967 41 4.000 70 1503.490 0.3 3.465 24 3.480 45 2023.374 2.7 3.375 39 3.390 35 3503.267 0.2 3.199 35 3.220 40 511Table 2: Chemical composition of the samples (EPMA).S1FeO K 2 O CaO Na 2 O SiO 2 Al 2 O 3 Sum0.45 1.17 3.77 2.74 68.52 13.09 89.810.20 0.93 3.78 2.69 68.72 13.50 90.050.30 0.58 4.05 2.59 69.16 13.35 90.210.57 0.67 5.02 2.17 66.93 14.22 90.550.42 0.59 4.20 2.42 68.40 13.42 90.5660www.sci.u-szeged.hu/asvanytan/acta.htm
Acta Mineralogica-Petrographica, Abstract Series 5, Szeged, 2006HEAVY METALS IMPACT ON PLANTS AT M<strong>IN</strong><strong>IN</strong>G AND RECOVERY DUMPS OFPOLYMETALLIC WASTE ORE MATERIAL <strong>IN</strong> <strong>THE</strong> SURROUND<strong>IN</strong>GS OF <strong>THE</strong>NEOVOLCANITES OF <strong>THE</strong> ŠTIAVNICKÉ VRCHY MTS. AREAKRIŽÁNI, I., ANDRÁŠ, P. & JELEŇ, S.Geological Institute, Slovak Academy of Sciences, Severná 5, 97401 Banská Bystrica, SlovakiaE-mail: andras@savbb.skThe most expressive manifestations of exploitation activitiesin mining regions are rests of mining dumps, which representdumping grounds of disintegrated rocks, fine-milledores and chemical matters used during the dressing activities.Until now these dumping grounds were perceived only as“memorials to the industry” or as anthropogenic reliefcreatingelements. Surroundings of Banská Štiavnica is a verygood model area in this respect. All this region was affectedby mining activity even during Antiquity (maybe even duringPrimeval Age).Vegetation at dumps of various age was investigated. Theoldest dumps from 14 th to 16 th centuries, worked as meadows,are covered by grass, which consists of species resistantagainst heavy metals: Alnus glutinosa, Acetosella vulgaris,Luzula campestris, Arrhenatherum elatius, Avenella flexuosa,Leucanthemum vulgare, Dianthus carthusianorum. Roveňdump from 18 th and 19 th centuries is predominantly plantedby trees Pinus nigra, Pinus sylvestris and more rarely byPicea abies. On the youngest dumps (Wolf and Michal)Betula pendula, Alnus glutinosa, Salix caprea and some otherplants subsist.The following evolutionary vegetation stages were recordedon dumps and soils influenced by heavy metal pollution:on dump areas with fine-grained substrate: Tussilagofarfara, Agrostis tenuis and Artemisia vulgaris, Daucus carotaand Tanacetum vulgare, while on places where morehumus is available, we can find the next species: Avenellaflexuosa, Nardus stricta, and mainly species from the surroundings:Arrhenatherum elatius, Veronica chamaedrys,Phleum pratense and Festuca rubra. The Fe, Mn, Cu, Zn, Pb,Cd, As and Hg contents in their dry tissues are presented inTable 1.Percolating acid waters intensively damage and destroythe whole biotope, contaminate underground waters by Zn,Cu, Cd, Fe, Bi, Mn. The result of biological-chemical processesis the biological transformation of the original sulphidesas well as of the alumosilicates. The comparison of heavymetal concentrations in Acetosella vulgaris from the olddumps and in Tussilago farfara from the youngest dumpsshow that the plants are contaminated by heavy metals andthat the contents in Acetosella vulgaris are much higher thanin Tussilago farfara. Both species are resistant to heavy metalpollution and are able adapt themselves to the strongly contaminatedsoils. According to BANÁSOVÁ et al. (1998) theplants can resist the toxic effect of heavy metals by two ways:1) they prevent heavy metal incorporation to the tissues (“exclusionmechanism”), e.g. Aldus glutinosa or 2) they convertthe metal within their cells to a less toxic form (“tolerancemechanism”).ReferenceBANÁSOVÁ, V., DANÁKOVÁ, A. & KRIŽÁNI, I. (1998):Bulletin Slovenskej botanickej spoločnosti, 20: 166–171.Table 1: Average contents (mg · kg –1 ) of selected heavy metals in dry tissuesof Tussilago farfara (Tf) and Acetosella vulgaris (Av)Tussilago farfaraAcetosella vulgarisElementdumpRoveňdumpLintichdump of theMichal aditdump of theNová shaftdumpRoveňdumpsWolfFe 169.00 344.00 644.00 280.00 173.00 634.00Mn 32.50 125.00 57.00 75.00 325.00 1 230.00Cu 13.00 15.00 11.00 20.00 5.00 22.00Zn 48.50 190.00 261.00 98.00 353.00 323.00Pb 13.50 24.00 37.00 21.00 6.00 47.70Cd 1.00 tr. 6.00 3.00 tr. 1.30As 0.41 0.44 0.43 0.45 0.49 0.45Hg 0.02 0.04 0.04 0.03 0.05 0.06www.sci.u-szeged.hu/asvanytan/acta.htm 61
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