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Rudarstvo 2011 / Mining 2011Slika 5. Majdan „Suljo Ĉilić― uzorak SC-47Krupna zrna bojenog minerala augita (ţuto i plavozeleno) u gabrovskoj osnovi. Rijedak biotit, braonboje. Lijevo u sredini ljubiĉaste boje olivin.Uzorak SĈ-41Radi se o izuzetno krupnozrnom uzorku koji se razlikuje od uzorka SĈ-30 po nešto većem sadrţajubojene komponente, prije svega biotita. Mikroskopska tj. optiĉka analiza pokazuje intenzivnealteracione procese na svim konstatiranim mineralnim vrstama. Tako su feldspati zamućeni savidljivim pertitom dok su od pojedinih kristala augita i biotita ostala samo recentna zrna ispunjenahloritom ili magnetitom (biotit) te epidotom, hloritom, uralitom, magnetitom (klinopiroksen) dok jeolivin samo kataklaziran. Prisutna je i naknadna silifikacija uz obaranje kvarca.Jednoosna ĉvrstoća na pritisak: 224MPaStruktura: Alotriomorfno zrnasta (gabrovska)Petro determinacija: Krupnozrni biotitsko-augitski gabroSlika 6. Majdan „Suljo Ĉilić― uzorak SC-41655
Rudarstvo 2011 / Mining 2011Tipiĉna krupnozrna gabrovska struktura od mreţe baziĉnih plagioklasa prizmatiĉnog presjekaizraţenih bliznih lamela, sa velikim zrnom biotita u gornjem lijevom dijelu slike. Dole desno rozetekristobalita, kao ilustracija sekundarne silifikacije i obrazovanja korozionih šupljina.Uzorak SĈ-30Preparat je izgraĊen od mreţe krupnozrnih baziĉnih plagioklasa sa augitom, bititom i olivinom umeĊuprostorima. Prisutni su i sekundarni procesi koji su oĉekivani i svode se na uralitizaciju ihloritizaciju klinopiroksena te opacitizaciju biotita.Jednoosna ĉvrstoća na pritisak: 247MPaStruktura: GabrovskaPetro determinacija: Krupnozrni augitsko-biotitski gabroSlika 7. Majdan „Suljo Ĉilić― uzorak SC-30Krupna zrna baziĉnog plagioklasa prizmatiĉnog presjeka (lijevo), sa velikim zrnima bliţnjenog augita,plavo, u desnom dijelu slike. Lijevo gore zrno biotita sa nejasnom braon bojom po rubu a ucentralnom dijelu zrno magnetita nastalo na raĉun alteracije primarnog minerala.Uticaj strukturne graĊe na ĉvrstoću gabraKod majdana „Suljo Ĉilić― gabro je izuzetno krupnozrn. Manje razlike izmeĊu uzoraka sa ovogmajdana javljaju se u kvantitativnom sadrţaju bojenih minerala prvenstveno biotita, kao i u stepenunjihove alteracije. Uzorak SĈ-30 (247MPa) je izgraĊen od relativno svjeţih plagioklasa što mu dajeveću ĉvrstoću. Alteracioni procesi su izraţeni preko pojave alteracije augita u hlorit, opacitizacijebiotita i pojave olivina u manjem procentu. Opacitizacija biotita napredovala je od ruba zrna ka centru.Plagioklasi u uzorku SĈ-41 (224MPa) su zamućeni dok su augit i biotit potpuno alterisani što u uzorkustvara oslabljene zone koje utiĉu na ĉvrstoću na pritisak uzorka. Kod uzorka SĈ-47 (208MPa) porednajveće dimenzije zrna, intenzivniji su procesi alteracija u odnosu na druga dva uzorka, što se ogleda upojavama sekundarnih alteracionih minerala magnetita, hlorita i epidota. TakoĊer, stepen alteracijeispucalih plagioklasa je veći u odnosu na druga dva uzorka (više ispucali, nagriţenih rubova) što,pored alteracija bojenih minerala, znaĉajno utiĉe na smanjenje ĉvrstoće.Iz analiza mjerenja jednoosne ĉvrstoće na pritisak gabra sa majdana „Suljo Ĉilić―, moţe se zakljuĉitida strukturna graĊa ima veliki uticaj na dobivene vrijednosti ĉvrstoće. Rasipanje rezultata ukazuje naneujednaĉenost strukturne graĊe, koja daje razliĉita otporna svojstva istom stijenskom materijalu656
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Page 662 and 663: σult (MPa)Rudarstvo 2011 / Mining
Page 666 and 667: Rudarstvo 2011 / Mining 2011ukoliko
Page 668 and 669: Rudarstvo 2011 / Mining 2011 Mokr
Page 670 and 671: Rudarstvo 2011 / Mining 2011kompres
Page 672 and 673: Rudarstvo 2011 / Mining 2011RAZVOJ
Page 676 and 677: Rudarstvo 2011 / Mining 2011Bio-reg
Page 678 and 679: Rudarstvo 2011 / Mining 2011Prednos
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Page 682 and 683: Rudarstvo 2011 / Mining 2011Table 5
Page 684 and 685: Rudarstvo 2011 / Mining 2011Bending
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Page 688 and 689: Rudarstvo 2011 / Mining 2011poznato
Page 690 and 691: Rudarstvo 2011 / Mining 2011Izuzetn
Page 692 and 693: Rudarstvo 2011 / Mining 2011skulptu
Page 694 and 695: Rudarstvo 2011 / Mining 2011Na osno
Page 696 and 697: Rudarstvo 2011 / Mining 2011Proseĉ
Page 698 and 699: Rudarstvo 2011 / Mining 2011Zaklju
Page 700 and 701: Rudarstvo 2011 / Mining 2011Analiza
Page 702 and 703: Rudarstvo 2011 / Mining 2011 Diskon
Page 704 and 705: Rudarstvo 2011 / Mining 2011UTICAJ
Page 706 and 707: Rudarstvo 2011 / Mining 2011Diskusi
Page 708 and 709: Rudarstvo 2011 / Mining 2011Zaklju
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stanje i perspektive u rudarstvu i odrÅ£ivi razvoj mining present state ...

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