ࡱ> G zbjbjَ 4IR3]8L44'FX&Z&Z&Z&Z&Z&Z&$) +~&}~&!!!!"X&X&!F!%V &@X&@L& The average structural density of barite crystals of different habit types Biserka Radanovi-Gu~vica Key words: barite, habit types, reticular density, average structural density of crystal Klju ne rije i: barit, tipovi habitusa, retikularna gustoa, srednja strukturna gustoa kristala Abstract Eight different habit types of barite crystals which could be classified in 4 essentially different groups were determined by morphological analysis: Eb group - barite crystals elongated in (010( direction; Ea group - barite crystals elongated in (100( direction; Tc group - barite crystals tabular on basal pinacoid (001(; Ec group - barite crystals elongated in (001( direction. By determination and comparison of average structural densities of different habit types of barite crystals it was establish the spans of their values from 276.1 to 495.8, and overlapping of values for Eb group with Ea group and Tc group with Ec group. The sequence of habit types, with regard to the decreasing of average structural density, i.e. the priority sequence of developing of barite crystal types, was determined: Eb group Ea group Tc group Ec group. __________________________________________________________________ Department of Mineralogy and Petrography, Croatian Natural History Museum, Demetrova 1, 10000 Zagreb, Croatia Sa~etak Morfoloakom analizom odreeno je 8 razli itih tipova habitusa baritnih kristala koji se mogu svrstati u 4 bitno razli ite skupine: Eb skupina - kristali barita izduljeni smjerom (010(; Ea skupina - kristali barita izduljeni smjerom (100(; Tc skupina - kristali barita plo asti po baznom pinakoidu (001(; Ec skupina - kristali barita izduljeni smjerom (001(. Odreivanjem i usporedbom srednjih strukturnih gustoa razli itih tipova habitusa baritnih kristala utvreni su rasponi njihovih vrijednosti od 276,1 do 495,8 , te su uo ena preklapanja vrijednosti za Eb i Ea skupine, kao i za Tc i Ec skupine. Utvren je redosljed tipova habitusa s obzirom na smanjenje srednje strukturne gustoe kristala tj. prioritetni slijed razvoja baritnih kristala: Eb skupina - Ea skupina - Tc skupina - Ec skupina. INTRODUCTION Crystals of one and the same mineral species can appear in different forms, i.e. habit types. Besides numerous researchers, KOSTOV (1966; 1969; 1970; 1975) has investigated the changes of mineral habit during the crystallization of a certain mineral species. He pointed at influence of crystalline structure (unit cell dimensions, nature of bonds in structure) and external conditions during growth (chemical composition of solution, supersaturation degree of solution, type of ingredients) on the change of crystal habit of one and the same mineral species. BRAVAIS (1866) has observed the evident dependence between reticular density and probability of appearance of certain crystal form. The forms which tend to occur most frequently on crystals are those with faces parallel to lattice planes that have a high reticular density (BRAVAIS, 1866). KRIVOVI EV (1971) was introduce the term  average structural density of crystal which define the total contribution of reticular density of all crystal form faces, and calculate their values for 3 generations of barite crystals from Belore ensko locality. The developing sequence of 3 generations of morphological different barite crystals is in accordance with decrease of average structural density of crystals (KRIVOVI EV, 1971). In consideration of this fact, it is possible to determine the sequence of developing of barite crystal types. Barite is one of the mineral species, which could have extremely different habit types. BRAUN (1932) has determined seven different habit types of barite crystals on the basis of detailed investigation of relation between morphological characteristics and mineral association. Some specimens of barite from Westmorland and County Durham in the north of England, show up to six changes of habit during growth, from the crystals elongated in (100( direction, through the crystals tabular on basal pinacoid {001}, to the crystals elongated in (010( direction (SEAGER & DAVIDSON, 1952). Similar sequence is described on barite crystals from Tjuja-Mujun mine (SOLODOVNIKOVA, 1927). KRIVOVI EV (1971) has separated 3 generations of different habit types of barite crystals from Belore ensko locality, and determined the sequence of developing from the prismatic crystals elongated in (010( direction, through the thick-tabular crystals elongated in (010( direction, to the crystals tabular on basal pinacoid. Inverse sequence of developing is determined on barite crystals from Krapinske Toplice (ZEBEC, 1976). Sequence from crystals tabular on basal pinacoid, through the crystals elongated in (100( direction, to the crystals elongated in (010( direction, was accompanied with change of genesis temperature and decrease of SrSO4 content (ZEBEC, 1976). Observations of phantoms and inclusions in crystals of barite from Muddy Creek, Colorado, suggest at least five episodes of crystal growth, with changes in morphology with respect to time (TRUEBE, 1981). Recently, researches are aim to determine the dependence of barite morphology on different controlled conditions during the experimental crystal growth (FERNANDEZ-DIAZ et al., 1990; PRIETO et al., 1992). Relative numerous barite specimens with different habit of crystals are stored at collection of Department of Mineralogy and Petrography of Croatian Natural History Museum in Zagreb. Due to that fact it was undertaken a systematic researches of barite morphology and reticular density of the crystal form faces with the hope to define the priority sequence of developing of barite crystals types, on the base of calculated values of average structural density of crystal. This paper was result of investigations performed as part of masters thesis Morphological and chemical features of barite selected from the collection of Croatian Natural History Museum in Zagreb (RADANOVI-GU}VICA, 1995). MATERIAL AND METHODS The crystals of barite from Mrzle Vodice locality in Gorski Kotar region, Sivac on mountain Petrova gora and Ri ice in Lika region from Croatia; }une in north-western Bosnia, valley of river Krivaja, Ma kara district, Veova a and environment of Kreaevo in central part of Bosnia and Pra a in eastern Bosnia; `uplja Stena on Avala hill and Veliki Majdan in Serbia and Stari Trg (Trep a) in Kosovo were elaborated in this paper. Under the research program, the morphological, as well as relevant crystallographic analyses of the barite crystals, were performed. Morphological analysis included: goniometric measurement of the crystals performed for the most part (62 crystals) on a Goldschmidt type two-circle reflecting goniometer and for the smaller number (5 crystals) on contact goniometer. On the basis of faces determination from a gnomon projection and by the help of data for barite by GOLDSCHMIDT (1897) and PALACHE et al. (1952) the construction of the parallel perspective drawings of measured crystals was done by the method described by TERPSTRA & CODD (1961) as well as the determination of the different habit types of the barite crystals. Crystallographic research was performed by the X-ray powder method on the Philips vertical X-ray goniometer with Cu Ksymbol 97 \f "Symbol" radiation and graphite monochromator. Standard conditions of recording were: 40 kV, 30 mA, 1o 2symbol 113 \f "Symbol"/min for the counter and 1 cm/min for the recording paper, in the angular region from 9o to 62o 2symbol 113 \f "Symbol". Barite X-ray diffraction pattern was indexed conformably to JCPDS card no. 24-1035. The unit cell dimensions are result of refinement by the method of least squares performed by the GITTER computer program (HUMMEL, 1982) on the base of 28 to 32 indexed diffraction lines. Reticular density of a certain crystal form is the ratio of number of all atoms in the section of a crystal structure defined by elementary parallelogram Shkl and interplanar spacing dhkl. The number of all atoms in a certain section was performed by the ATOMS computer program (DOWTY, 1991) which give us the display of structure based on the data (coordinate system, unit cell parameters, space-group symmetry, atom coordinates). The data according to HILL (1977) are used for the display of barite structure. The surface of the elementary parallelogram was calculated according to formula: S2hkl = h2S2100 + k2S2010 + l2S2001 + 2(hkS100S010cossymbol 110 \f "Symbol" + klS010S001cossymbol 108 \f "Symbol" + lhS001S100cossymbol 109 \f "Symbol" (Shkl - surface of the elementary parallelogram of the face (hkl) in (2(; S100 = b0c0sinsymbol 97 \f "Symbol", S010 = c0a0sinsymbol 98 \f "Symbol", S001 = a0b0sinsymbol 103 \f "Symbol" (a0, b0, c0 - unit cell dimension in ((; symbol 97 \f "Symbol", symbol 98 \f "Symbol", symbol 103 \f "Symbol" - angles between crystal axes); symbol 110 \f "Symbol" = (100) ( (010); symbol 108 \f "Symbol" = (010) ( (001); symbol 109 \f "Symbol" = (001) ( (100)) (PHILLIPS, 1946)). This formula is simplify since barite is orthorhombic: S2hkl = h2b20c20 + k2c20a20 + l2a20b20 According to KRIVOVI EV (1971) the average structural density of crystal ECR was calculated according to formula: ECR = ( (M x E hkl) (M is the morphological persistence of certain crystal form (FRANK-KAMENECKII, 1951), Ehkl is the reticular density of a certain crystal form in [number of atoms in 3], and product M x E hkl define the contribution of reticular density of certain crystal form in total structural density of crystal). Morphological persistence is the ratio of total surface of all faces of a certain crystal form and surface of whole crystal, and was expressed in percent. M is calculated thus face surfaces of emphasized crystal forms were measure on several crystals of a certain habit type, and it was calculated the average value of this surfaces for a respective crystal form. Barite specimens, on which were performed aforesaid researches, are stored at collection of Department of Mineralogy and Petrography of Croatian Natural History Museum in Zagreb. 3. RESULTS 3.1. MORPHOLOGICAL ANALYSIS By morphological analysis of barite crystals from 12 localities, 8 different habit types were determined. Those habit types could be classify in 4 essentially different groups: Eb group of barite crystals (Tab. 1) is represented by 2 habit types elongated in symbol 91 \f "Symbol"010symbol 93 \f "Symbol" direction. One habit type was noticed only in `uplja Stena, and was described before (BARI, 1949). These columnar crystals have dominant {101} and somewhat smaller {011} form faces. According to Braun s classification, this habit type is intermediate between ore  IIIb type  Pb001[010] and carbonate  IVa type Ab (BRAUN, 1932). Another habit type was observed in Veliki Majdan. These columnar crystals have well-formed {001} and {101} faces, and somewhat smaller {011} and {210} form faces, and corresponds to carbonate IVa type Ab (BRAUN, 1932). Ea group of barite crystals (Tab. 2) is represented by 2 habit types elongated in symbol 91 \f "Symbol"100symbol 93 \f "Symbol" direction. One habit type was noticed in Ri ice and Kreaevo (Raatelica, Dubrave, Dusina). These thick-tabular crystals have emphasized {001}, {011} and {101} form faces, and corresponds to rectangularly-tabular  I type  Pa001[100], [010] (BRAUN, 1932). Another habit type was observed only in Ma kara district. These columnar crystals have well-formed {001}, {011}, {101} and {210} form faces, and corresponds to carbonate - IVb type  Aa (BRAUN, 1932). Tc group of barite crystals (Tab. 3) is represented by 2 habit types tabular on symbol 123 \f "Symbol"001symbol 125 \f "Symbol" basal pinacoid. One habit type was noticed only in }une. These tabular crystals have well-formed face from the [100] and [010] crystallographic axe s zones and specially emphasized {011} and {101} form faces. Another habit type was the most frequent type, and was found on the following localities: Mrzle Vodice, }une, Veova a, Kreaevo, Pra a, Veliki Majdan and Stari Trg (Trep a). This habit type of barite crystals in Stari Trg (Trep a) was described before (BARI, 1948). These tabular crystals have marked {210} form faces, and corresponds to silicate  VI type  Pb001[010] (BRAUN, 1932). Ec group of barite crystals (Tab. 4) is represented by 2 habit types elongated in symbol 91 \f "Symbol"001symbol 93 \f "Symbol" direction. One habit type was observed only in Sivac. These crystals have well-formed {410} and {100} faces and somewhat smaller {001} and {210} form faces, and corresponds to Wolnyn VII type Ac (BRAUN, 1932). Another habit type was noticed only in Krivaja. These isometric to elongated crystals have dominant {210} form faces and somewhat less emphasized {001}, {101} and {211} form faces, and corresponds to cubic-pyramidal V type I001,210[120] (BRAUN, 1932). Detailed review of results of morphological analysis was given in article  A new crystallographic feature of barite from the Balkan Peninsula (RADANOVI-GU}VICA et al., 1999) accepted for print in Neues Jahrbuch fr Mineralogie. 3.2. AVERAGE STRUCTURAL DENSITY OF BARITE CRYSTALS The average structural density of crystal was calculated according to aforesaid procedure for 14 barite samples, e.g. 8 different habit types of crystals (Tab. 1 - 4). Values of average structural density of crystal are greatest in the case of barite crystals elongated in [010] direction, and amounts 419.5 to 495.8 (Tab. 1). Barite crystals elongated in [100] direction have the values of average structural density in relatively small range from 415.8 to 431.3 (Tab. 2). Values of average structural density of barite crystals tabular on basal pinacoid {001} amounts 346.3 to 394.1 (Tab. 3). Values of average structural density of crystal are smallest in the case of barite crystals elongated in [001] direction, and amounts 276.1 to 349.4 (Tab. 4). The ranges of values of average structural densities of 4 main groups of barite crystal habit types were shoved on figure 1. The overlapping of Eb group (barite crystals elongated in [010] direction) with Ea group (barite crystals elongated in [100] direction) was observed, as well as Tc group (barite crystals tabular on symbol 123 \f "Symbol"001symbol 125 \f "Symbol" basal pinacoid) with Ec group (barite crystals elongated in symbol 91 \f "Symbol"001symbol 93 \f "Symbol" direction). Besides, it is necessary to accentuate that the value of average structural density of columnar barite crystals, elongated in symbol 91 \f "Symbol"010symbol 93 \f "Symbol" direction, with well-formed {101} and {001} faces, as well as with somewhat smaller {210}, {201} and {011} form faces, which were noticed in Veliki Majdan mine is very close to value of average structural density of columnar crystals elongated in symbol 91 \f "Symbol"100symbol 93 \f "Symbol" direction, with well-formed {011} and {001}, as well as with somewhat smaller {101} and {210} form faces, from Ma kara district. According to Braun s classification, the both habit types corresponds to carbonate type, i.e. the crystals elongated in symbol 91 \f "Symbol"010symbol 93 \f "Symbol" direction are carbonate IVa type - Ab, and the crystals elongated in symbol 91 \f "Symbol"100symbol 93 \f "Symbol" direction are carbonate IVb type Aa (BRAUN, 1932). CONCLUSIONS By comparison of the values of average structural densities of different habit types of barite crystals, the sequence of developing of barite crystal types in consideration to decrease of average structural density, was determined. In general, the priority sequence was: barite crystals elongated in [010] direction (Eb group) barite crystals elongated in [100] direction (Ea group) barite crystals tabular on symbol 123 \f "Symbol"001symbol 125 \f "Symbol" basal pinacoid (Tc group) barite crystals elongated in [001] direction (Ec group) (Fig. 1). The overlapping of ranges of values of average structural density for Eb group (barite crystals elongated in [010] direction) and Ea group (barite crystals elongated in [100] direction) was observed, as well as for Tc group (barite crystals tabular on symbol 123 \f "Symbol"001symbol 125 \f "Symbol" basal pinacoid) and Ec group (barite crystals elongated in symbol 91 \f "Symbol"001symbol 93 \f "Symbol" direction) (Fig. 1). On the base of previous researches about the sequence of developing of barite crystal types (SOLODOVNIKOVA, 1927; SEAGER & DAVIDSON, 1952; KRIVOVI EV, 1971; ZEBEC, 1976), as well as the research preformed in this paper, it is possible to conclude that the sequence of developing of barite crystal types is not strictly defined, already, is changeable (alternate) from case to case. Besides the density of atomic arrangement, which defined the sequence of developing of crystal habit types, there are a many others factors, which are able to cause the change in sequence, even more the change of direction. Acknowledgments I would like to thank academician Stjepan `avni ar for his helpful and expert advises during the elaboration of master s thesis, and comments on manuscript. 5. REFERENCES BARI, Lj. (1948): Barit iz rudnika Trep e (La baryte des mines de Trep a).- Glasnik Prir. Muzeja Srp. Zemlje (Bull. Museum d Hist. nat), Ser. A, 1, 71-79. BARI, Lj. (1949): Nekoliko rije i o obliku baritnih kristala odnosno njima korespondentnim aupljinama u kremenom materijalu sa `uplje Stene na Avali nedaleko Beograda (Quelques remarques sur la forme des cristaux de baryte, ou des cavits correspondantes, dans les quartz de `uplja Stena dans l Avala, aux environs de Belgrade).- Geol. anali Balkan. Pol., 17, 66-72. BRAUN, F. (1932): Morphologische, genetische und paragenetische Trachtstudien an Baryt.- Neues Jahrbuch Miner. Abh., 65, 173-222. BRAVAIS, M.A. (1866): tudes Crystallographiques.- Gauthier-Villars, Paris. DOWTY, E. (1991): ATOMS - A Computer Program for Displaying Atomic Structures, ibm-pc Version 2.1, Kingsport. FERNANDEZ-DIAZ, L., PUTNIS, A. & CUMBERBATCH, J. (1990): Barite nucleation kinetics and the effect of additives.- Eur. J. Mineral., 2, 495-501. FRANK-KAMENECKII, V.A. (1951): Mineralogija i kristalografija barita iz ~il v verhovijah reki Kubanji.- Zap. Vses. Miner. Obshch., 80, 33-47. GOLDSCHMIDT, V. (1897): Krystalographische Winkeltabellen, Verlag von Julius Springer, Berlin, p. 60-62. HILL, R.J. (1977): A further refinement of the barite structure.- Can. Mineral., 15, 522-526. HUMMEL, W. (1982): Bestimung von Gitterparametern aus Pulverdiagrammen, Tbingen. KOSTOV, I. (1966): Veranderungen des Kristallhabitus von Mineralen mit Rutil-Struktur.- Ber. deutsch. Ges. geol. Wiss., 11, 295-304. KOSTOV, I. (1969): Habit types and crystallogenesis of diaspore and goethite.- Annuaire de lUniversite de Sofia, 61, 167-176. KOSTOV, I. (1970): Habitusi i genezis polimorfnih modifikacii Al2SiO5.- Problems of petrology and genetic mineralogy, Sobolev s vol. II, 157-160. KOSTOV, I. (1975): Apophyllite Morphology as an Example of Habit Modification of Planar Crystals.- Neues Jahrbuch Miner. Abh., 123/2, 128-137. KRIVOVI EV, V.G. (1971): K kristallomorfologiji barita Belore enskogo mestoro~denija.- Zap. Vses. Miner. Obshch., 100, 462-470. PALACHE, C., BERMAN, H. & FRONDEL, C. (1952): The System of Mineralogy, Vol. II, 7th edition, John Wiley & Sons, Inc., Chapman and Hall, LTD, New York - London, p. 408-415. PHILLIPS, F.C. (1946): Crystal Habit in: An Introduction to Crystallography.- Longmans, Green and Co Ltd, London, 295-311. PRIETO, M., PUTNIS, A., ARRIBAS, J. & FERNANDEZ-DIAZ, L. (1992): Ontogeny of baryte crystals grown in a porous medium.- Miner. Mag., 56, 587-598. RADANOVI-GU}VICA, B. (1995): Morfoloake i kemijske zna ajke barita odabranih iz zbirke Hrvatskog prirodoslovnog muzeja u Zagrebu (Morphological and chemical characteristics of barite selected from the collection of Croatian Natural History Museum in Zagreb).- Magistarski rad, Prirodoslovno-matemati ki fakultet Sveu iliata u Zagrebu, 152 str. RADANOVI-GU}VICA, B., `AVNI AR, S. & ZEBEC, V. (1999): A new crystallographic feature of barite from the Balkan peninsula.- Neues Jahrbuch Miner., in press. SEAGER, A.F. & DAVIDSON, W.F. (1952): Changes in habit during the growth of baryte crystals from the north of England.- Miner. Mag., 29, 885-894. SOLODOVNIKOVA, L.L. (1927): Bariti Tjuja-Mujunskogo rudnika.- Trudi Min. muzeja AN SSSR, 2, 37-90. TERPSTRA, P.D. & CODD, L.W. (1961): Crystallometry.- Longmans, London, 420 p. TRUEBE, H.A. (1981): Water-clear barite from Muddy Creek, Colorado.- Miner. Record, 12, 79-80. ZEBEC, V. (1976): Barit i kalcit iz kamenoloma litotamnijskog vapnenca u Krapinskim Toplicama u Hrvatskom Zagorju (Baryt und Calcit aus dem Leithakalksteinbruch in Krapinske Toplice in Hrvatsko Zagorje (Kroatien, Jugoslawien)).- Geoloki vjesnik, 29, 323-345. PAGE 2 PAGE 7 PAGE  PAGE 7 #$'(56ijmnqru v T U V _ ` a j k l u v w   v x ~ dflntvtv~CJEH CJEHH* j}CJ j{CJ j]CJ j[CJCJH*CJEH5CJCJQDFX~ / 0 1  )*78!"$@&B&l& & F$DFX~ / 0 1  )*78!"$@&B&l&n&)i*,N/1A2245668i9j9u9v999::>>CCFIHILMMMNNNQXXXXZ[]a a0acc0c2cjdldfLgNg)h*hvhwhhhiviwijkkk     _|~ "(* M!N!1-2-G-I--------.. .!.#.$.:.<.//0 01111111111111111111111 CJEHH*CJEH CJEHH* jCJUCJEHjCJEHU j]CJ j[CJCJCJH*Nl&n&)i*,N/1A2245668i9j9u9v999::>>CCFIHILM111111111111222 2!2$2'2(2>2@2C2F22222222222222222222222222222222223333 3 333*3+3,3-3/303E3G3I3J3_3a3c3d3z3|333333 j]CJ@CJH*mH j[CJ jCJUCJ CJEHH*U333333333344*4,4444444444444444455555555555555566 6 666n6q66666::.;0;Z;^;d;f;;;===> >>>>>K?L?a? CJEHH*CJH* jSCJCJH*@CJH*mH@CJH*mH @CJmH jCJUCJ jCJNa?c?f?g?|?@AAApCrCCC4D6DbDfDlDnDDDIIIJILIII JJJJ'J)JJJKKQQQQ4R5RXRYRoRqRtRuRRRRRRRRRRRRRSSSSSSSSfUhUUUUUUUWWWWWWXX:X;X[X\XqXsX CJEHH*CJH*CJH*CJ jCJU[MMMNNNQXXXXZ[]a a0acc0c2cjdldLgNg)h*hvhwh & FsXvXwXXXXXZZZMZNZOZsZtZZZZZZZZZZZZZQ[R[[[[[ \\:\>\D\F\r\v\\\\\]]$]&]P]T]mmmmPqTqzzzzzzzzzzzzzzzzzzzzzzzzzzzz0JmH0J j0JUCJH*CJEH CJEHH*CJH* jCJUCJTwhhhviwikkkkWlXlll0m1mmmnnoopprrrrssvk kkkWlXlll0m1mmmnnooppqrrrrrsssvvwwxxxxx?y@yyyzzzzzzzzzzzzzzzzzzzz   ;vvwwxxxx?y@yyyzzzzzzzzzzzzzzzh&`#$h&`#$zz2 00&P P. A!"#P$%@ [4@4NormalCJOJQJkHmH >@> Heading 1$$d@&5CJ<A@<Default Paragraph Font, @,Footer  !&)@& Page Number,@,Header  !0B@"0 Body TextdCJ@ @@Index 1:dCJOJQJmH$/@R$List }R %222513a?sXzNQSTUWl&MwhvzzORVXZ[kzPYy+!B!C!T!k!l!}!!!!"""/"0"A"X"Y""""""""""" # ##5#6#I#`#a#()))))++++++-.. .!.".000000,8C8D8H8_8`8888888\9r9s9w999::::::;;;;;;/<E<F<J<`<a<G>^>_>c>z>{>???? @@K@a@b@f@|@}@}R99999999999999999999999999999999999999999 !%,.5!!t!!Uf!46`hprtvSU^`iktv %18:EFNOWXZ]ghnowx !)+,36>?EFNOQRXYbjlmtw !"-.0BDEGHNOZ[fgijlmnoqry{~  %')*1467>ACDKNPQX + Z d  [fmz!&W_ jpSY\m #MTV]ho8C_i #*s}JPci@CHS]` !!!(!+!G!J!Q!T!p!s!z!}!!!!!!!##########/$2$Y$\$h$k$$$$$*%-%''((O)U)V)[)w)|)+*/*7*<*R*U*]*_*****1+4+<+>++, ,,,,,$,&,,,,,,,,-----*.2.W.[.O/T/U/[/]/a/c/j/l/s/u/z/|//////////////////]0b0-1211112e3v3333333336 6h8p8:#:$:*:*;1;<< <<}<<<<== >">>>>>>>@@@@A A A*A2A7A'C.C/C8CCCCCCCCCCCCCCCCCCCDDD DDDDDD D/D5D7D:D=D@DPDUDWDYDcDkDlDrDuD{D|DDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDEE E EEEEEEE%E)E/E1E3E4E7E8E?E@EOEQEUEVEYEdEjEkEpEqEuEvE}EEEEEEEEEEEEEEFFFFFFF F(F0F3FDFKFMFPFZF`FaFtFwFFFFFFGG!G,GrGuGGGGGGGGGGGGGGGGGGGGGGGGH HH H+H8HJHKHYH[HaHbHeHmHuHHHHHHII I IIIII/I1I9IKFKNKQKeKoKqKtKKKKKKKKKKKKKKKLLLLLLLLMMM#M)M0MRMZM^MdMMMMMMMMMMMMMMMMMMMMMMNNNNNN%NNNNNNNNNNNNNNNNNNOOO%O*O|OOOOOOOOOOP P1P>P@PCPMPSPTPdPePlPoPtPzPPPPPPPPPPPPPPPPPPPPDQIQVQ[Q\Q]Q^QdQeQgQhQrQsQQQQQQQQQQQQQQQQQQQQQQQQQQQQQRR RRRR$R)R1R2R9RIR{R~R,::A! , x  8##/$7$m$%n(v((*)7*=*O++&,,,,,--////]0c0x0141C122w3y3444466888;;>>?#?@BCC7D:DBDNDEEEEFF3F5FtFvFoGqGGGGHH HHHHHHHIIIIIIIIJJJJ5K7KQKSKKKKKKKKKL-LLLMMMMNNyO{OPPP/PlPnPPP&Q(Q0QBQ&R(RIR{R~RPrivate(C:\DOS\AutoRecovery save of BARITEGC.asdPrivateA:\BARITEGC.DOC Goran Guzvica1C:\WINDOWS\TEMP\AutoRecovery save of BARITEGC.asd Goran Guzvica1C:\WINDOWS\TEMP\AutoRecovery save of BARITEGC.asd Goran Guzvica1C:\WINDOWS\TEMP\AutoRecovery save of BARITEGC.asd Goran GuzvicaA:\BARITEGC.DOCPrivateA:\BARITEGC.DOC Goran GuzvicaA:\BARITEGC.DOC Goran GuzvicaA:\BARITEGC.DOCBiserkaC:\My Documents\BARITEGC.docߞ4|q C_' hh.hho(.hho(.4|qC_'@HRHR\tHRHRx11 VVV#V$V(V*+-0239;?ACFGHJLMO}RPP@P P$@PP4@PP@@P&PT@P4Pl@P:P|@P@PDP@PLP@PTP@P\P@PbP@PjP@PnP@PtP@G:Times New Roman5Symbol3& :Arialc\t(normal text)Times New Roman"CV KK$5& C"YV 20dRS$CRYSTALLOGRAPHICAL AND MORPHOLOGICALsgBiserka Oh+'0  4 @ L Xdlt|%CRYSTALLOGRAPHICAL AND MORPHOLOGICALft RYSsgSgSNormalLBiserka2seMicrosoft Word 8.0A@@p@ij@ij C ՜.+,D՜.+,T hp  Private"RS  %CRYSTALLOGRAPHICAL AND MORPHOLOGICAL Title 6> _PID_GUIDAN{ED3B4384-A3C3-11D2-8117-0040055467C0}  !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\^_`abcdefghijklmnopqrtuvwxyz|}~Root Entry F`h1Table]+WordDocument4SummaryInformation(sDocumentSummaryInformation8{CompObjj  FMicrosoft Word Document MSWordDocWord.Document.89q