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178

Raeosavljevi~ s 1977 Mlneralne parageneze rudnlh Iea u Cumavl~ima Stru~nl rad FSD Srebreniee

RadosavlJevl~ s Rakl~ S Strumberger V Dimitrijevl~ R CvetkOli~ LJ 1986 Minerali srebra Iz Pb-Zn lel~ta Podrinjske metalogenetske oblasti XI KorgGeel Jug knJ 4 s 77-88 Tara

Radosavljevl~ s 1988 Mlneralogenetske karakterlsUke srebra u Pb-Zn leI~Uma ~oshydrlnJske oblasti Manuskrlpt - doktorska teza FSD ITNMS i RGF Beograd

Radosavljevi~ s 1990 Studlja rasp odele Au I Ag u rudnim Ieama rudnog polja Sreshybrenlce FSD Rudnlka Srebrenlce I ITNMS - Beograd

Rakl~ s 1962 Klaslflkaclja genetskih tlpova Pb-Zn lel~ta tercijamog magmatlzma Dlnarldii na osnovu karakterlstlka mineralnih parageneza Ref V Savet deo II s 189-195

Rakl~ s 1970 Izvdtaj 0 mikroskopsklm ispltivanjlma rudnih preparata podru~ja rushydnlka Srebrenlce FSD Srebrenlce

Rakl~ S DImitrlevl~ R Radosavljevl~ s 1978 Sulfosoli Srebrenlce BulanerltshySemselt - DemsonJt IX Kong Geol Jug s 386-390 Saraevo

Ramdohr P 1980 The ore mlrerals and their Intergrowths Pergamon Press

Ramoi~ M 1963 Rudne parageneze u oblasti Srebrenlce (Isto~na Bosna) Pos iZdashynle Geel glasnlka knj I Sarajevo

Tananeva AG Tomsen HI 1973 D Izdvajanjlma plutonskih i vulkanogenlh t1pova kalajnlh orudnjenja Geel rud mest tom XV No 3 Moskva

TopalOli~ D 1984 Li~na Sb-Pb-Zn orudnjenjc Cumal~a (Rudnl rejon Srebreniee) Rad Geoinstituta knj 17 s 77-87 Beograd

Vandjel V 1978 Srpsko-makedonska metalogenetska zona najzna~ajnije olovo-eishynkovo podru~je Jugoslavlje II Savet 0 Pb-Zn lei~tlma poundFRJ SUp

Vuk~inOlI~ s 1978 Razlomi centrl magmatske akUvnosU i rudno perspektivni teshyren ~ireg podropoundja Srebrenlee na osnovu aeromagnetnih podataka II Sashyvet 0 Pb-Zn leIsectUma fFRJ Stlp

179

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178

Raeosavljevi~ s 1977 Mlneralne parageneze rudnlh Iea u Cumavl~ima Stru~nl rad FSD Srebreniee

RadosavlJevl~ s Rakl~ S Strumberger V Dimitrijevl~ R CvetkOli~ LJ 1986 Minerali srebra Iz Pb-Zn lel~ta Podrinjske metalogenetske oblasti XI KorgGeel Jug knJ 4 s 77-88 Tara

Radosavljevl~ s 1988 Mlneralogenetske karakterlsUke srebra u Pb-Zn leI~Uma ~oshydrlnJske oblasti Manuskrlpt - doktorska teza FSD ITNMS i RGF Beograd

Radosavljevi~ s 1990 Studlja rasp odele Au I Ag u rudnim Ieama rudnog polja Sreshybrenlce FSD Rudnlka Srebrenlce I ITNMS - Beograd

Rakl~ s 1962 Klaslflkaclja genetskih tlpova Pb-Zn lel~ta tercijamog magmatlzma Dlnarldii na osnovu karakterlstlka mineralnih parageneza Ref V Savet deo II s 189-195

Rakl~ s 1970 Izvdtaj 0 mikroskopsklm ispltivanjlma rudnih preparata podru~ja rushydnlka Srebrenlce FSD Srebrenlce

Rakl~ S DImitrlevl~ R Radosavljevl~ s 1978 Sulfosoli Srebrenlce BulanerltshySemselt - DemsonJt IX Kong Geol Jug s 386-390 Saraevo

Ramdohr P 1980 The ore mlrerals and their Intergrowths Pergamon Press

Ramoi~ M 1963 Rudne parageneze u oblasti Srebrenlce (Isto~na Bosna) Pos iZdashynle Geel glasnlka knj I Sarajevo

Tananeva AG Tomsen HI 1973 D Izdvajanjlma plutonskih i vulkanogenlh t1pova kalajnlh orudnjenja Geel rud mest tom XV No 3 Moskva

TopalOli~ D 1984 Li~na Sb-Pb-Zn orudnjenjc Cumal~a (Rudnl rejon Srebreniee) Rad Geoinstituta knj 17 s 77-87 Beograd

Vandjel V 1978 Srpsko-makedonska metalogenetska zona najzna~ajnije olovo-eishynkovo podru~je Jugoslavlje II Savet 0 Pb-Zn lei~tlma poundFRJ SUp

Vuk~inOlI~ s 1978 Razlomi centrl magmatske akUvnosU i rudno perspektivni teshyren ~ireg podropoundja Srebrenlee na osnovu aeromagnetnih podataka II Sashyvet 0 Pb-Zn leIsectUma fFRJ Stlp

179

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000

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LIOLI r CJ

o r

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1 0 0 000 0 0 0 0 0 0 0 0 0 D 0 OrlltCJCJrrrCJrrrCJrCJCJr

r

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r r r

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r

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1 CJ

1 1ltLItCJLICJ~CJ0 co 1lt Ilt~~~ ~llill r r r r r r rII

186

Sm-fMARY

HYDRCYlHEID-lAL ALTERATIONS IN PART OF THE ORE DEPOOIT ALSAR

BBoev Faculty Oef Geology and Minig Stip TSerafimovski Faculty of Geology and Miming Stip SPetrov University of Sofia

The polymetalic ore deposit of antimony arsenic Thallium gold and some others Alssr is situated within the Kozu volcanic region Ore mineralisation of Sb As and Tl is mostly at the contact between the volcanic rocks and the carbonate rocks while the gold be aring mineralisation is basicaly controlled by the areal distrubution of the silification as a hydrotermal alteration The aim of this work is to present the hydrothermal alterations in part of the deposit mainly in the northern part Here the hydrothermal alterations are represented by silification dolomitisation kaolinisation pyritisation pyrofilitisation and 80 on

n H T EPA T Y P A

BBoeB neTpoAomKR reoxeuRjcKu R BynKsHonomKH KspsKTepRcTHKH HS BynKsHcKwTe CTeHH OA Kozyt nnSHMHS I 1988 I BOKTOPCKS ARcepTauRja

~HBaHoB UeTsnoreHRja jyxHor nen BSpAspcKe aOHe I 1965 I BOKTOPCKS BRcepTaURjs

187

Autor Bugarin Mile

GEOLoSKA PROBLEIlATlKA PRI ISTRAZrVANJU ZLATONOSNO-KVARCNIH ZrCA U RUDNOII POWU BLAGOJEV KAMEN

U V 0 D

Rudno polje blagojev Kamen nalazi se u istocnoj Srbiji i zahvashy

ta podrucje od Dunava na severu do Debelog Luga na jugu u duzishy

ni od 25 km i sirin1 3-5 km

Pomenuto rudno polje o~uhva-

tastene vulkanogeno sedimeshy

ntnog porekla staropalezojshy

ske starosti duz kojih je

mestimicno javljaju proboji

plagiogranita gabrova anshy

dezita i drugih magmatskih

stena Fizicke karakteristishy

ke magmatskih stena dosta su

izmenjene (metamorfisane) a

u pojedinim delovima vulkashy

nogeno sedimentne serije zashy

uzimaju poloiaj kao tektonshy

ski uklopci eela vendsko-koshy

mbrijska serija zauzima poloshy

zaj antiklinale cija anveloshy

pa ima tendenciju neizmenicshy

nag uzdizanja i spuitanja

sa razlicitim stepenom eroshy

zije U toj strukturi smesshy

tene su brojne kvarcne fice

sa razlicitim stepenom orudshy

njenja u pogledu zlata vo1shy

frama i srebra

Stepen koncentracije kvarcnih

IIbull

Institut za bakar Bor Slika 1

L_J___

184 a c c

=

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CKnK~KX8uRj8T8 e H8nozeH8 H8 ~onOMKTK38uKjaT8 K T8e SCymHOCT npe shyH

n CT8SYS8 nOQSTOK H8 rn8BH8T8 ~838 H8 MKHep8nK38UKj8T8 ~ IIICKnK~KK8UKj8T8 e npenCT8seH8 CO CKTHR ZKnKQKK H8 KS8PU 8 SO Hexo ~

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H8 nos eKe MeCT8 38e~HO CO cKn~KKauKj8T8 KM8Me npKcycTBO K H8 CKTHo3pHecT 6KOTKT

185 LIOLI LIOLIOO LIOLI 000 1lt Ilt CJ CJIltCJIltIlt CJ 1lt 1lt 1 1lt CJ 1lt

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r

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o 0 CJ LI 0

1 1lt LI LI LI LI 1 r LI CJ OOLIOCJ~ o CJ r r r

000 000 0 0 0 0 0 0 0 0 0 0000000 0 0 0 0 0 0 000 0 o OLIrLIO OCJ OrLILIr OCJrCJ~ r r r r r r

000 0 r ~ CJ CJ 0 0 0 0 0 000 000~ r CJ r LICJrJo~~CJCJrCJr

r r r

IIl o 0g o 0 r o 0 r r

oI~ CJ 0 ILIILI rLIO o 0cl o CJ r r

r

~ DCO CJ rO DCD 1lt LI t o CJ t1 1lt 0 t1 0 C--~~CJj LI t1III

Q r r t r IJ r r CJ r ~~ CODr r DCD 1 1 l shy nlA~cAJl CJ

1 CJ

1 1ltLItCJLICJ~CJ0 co 1lt Ilt~~~ ~llill r r r r r r rII

186

Sm-fMARY

HYDRCYlHEID-lAL ALTERATIONS IN PART OF THE ORE DEPOOIT ALSAR

BBoev Faculty Oef Geology and Minig Stip TSerafimovski Faculty of Geology and Miming Stip SPetrov University of Sofia

The polymetalic ore deposit of antimony arsenic Thallium gold and some others Alssr is situated within the Kozu volcanic region Ore mineralisation of Sb As and Tl is mostly at the contact between the volcanic rocks and the carbonate rocks while the gold be aring mineralisation is basicaly controlled by the areal distrubution of the silification as a hydrotermal alteration The aim of this work is to present the hydrothermal alterations in part of the deposit mainly in the northern part Here the hydrothermal alterations are represented by silification dolomitisation kaolinisation pyritisation pyrofilitisation and 80 on

n H T EPA T Y P A

BBoeB neTpoAomKR reoxeuRjcKu R BynKsHonomKH KspsKTepRcTHKH HS BynKsHcKwTe CTeHH OA Kozyt nnSHMHS I 1988 I BOKTOPCKS ARcepTauRja

~HBaHoB UeTsnoreHRja jyxHor nen BSpAspcKe aOHe I 1965 I BOKTOPCKS BRcepTaURjs

187

Autor Bugarin Mile

GEOLoSKA PROBLEIlATlKA PRI ISTRAZrVANJU ZLATONOSNO-KVARCNIH ZrCA U RUDNOII POWU BLAGOJEV KAMEN

U V 0 D

Rudno polje blagojev Kamen nalazi se u istocnoj Srbiji i zahvashy

ta podrucje od Dunava na severu do Debelog Luga na jugu u duzishy

ni od 25 km i sirin1 3-5 km

Pomenuto rudno polje o~uhva-

tastene vulkanogeno sedimeshy

ntnog porekla staropalezojshy

ske starosti duz kojih je

mestimicno javljaju proboji

plagiogranita gabrova anshy

dezita i drugih magmatskih

stena Fizicke karakteristishy

ke magmatskih stena dosta su

izmenjene (metamorfisane) a

u pojedinim delovima vulkashy

nogeno sedimentne serije zashy

uzimaju poloiaj kao tektonshy

ski uklopci eela vendsko-koshy

mbrijska serija zauzima poloshy

zaj antiklinale cija anveloshy

pa ima tendenciju neizmenicshy

nag uzdizanja i spuitanja

sa razlicitim stepenom eroshy

zije U toj strukturi smesshy

tene su brojne kvarcne fice

sa razlicitim stepenom orudshy

njenja u pogledu zlata vo1shy

frama i srebra

Stepen koncentracije kvarcnih

IIbull

Institut za bakar Bor Slika 1

L_J___

186

Sm-fMARY

HYDRCYlHEID-lAL ALTERATIONS IN PART OF THE ORE DEPOOIT ALSAR

BBoev Faculty Oef Geology and Minig Stip TSerafimovski Faculty of Geology and Miming Stip SPetrov University of Sofia

The polymetalic ore deposit of antimony arsenic Thallium gold and some others Alssr is situated within the Kozu volcanic region Ore mineralisation of Sb As and Tl is mostly at the contact between the volcanic rocks and the carbonate rocks while the gold be aring mineralisation is basicaly controlled by the areal distrubution of the silification as a hydrotermal alteration The aim of this work is to present the hydrothermal alterations in part of the deposit mainly in the northern part Here the hydrothermal alterations are represented by silification dolomitisation kaolinisation pyritisation pyrofilitisation and 80 on

n H T EPA T Y P A

BBoeB neTpoAomKR reoxeuRjcKu R BynKsHonomKH KspsKTepRcTHKH HS BynKsHcKwTe CTeHH OA Kozyt nnSHMHS I 1988 I BOKTOPCKS ARcepTauRja

~HBaHoB UeTsnoreHRja jyxHor nen BSpAspcKe aOHe I 1965 I BOKTOPCKS BRcepTaURjs

187

Autor Bugarin Mile

GEOLoSKA PROBLEIlATlKA PRI ISTRAZrVANJU ZLATONOSNO-KVARCNIH ZrCA U RUDNOII POWU BLAGOJEV KAMEN

U V 0 D

Rudno polje blagojev Kamen nalazi se u istocnoj Srbiji i zahvashy

ta podrucje od Dunava na severu do Debelog Luga na jugu u duzishy

ni od 25 km i sirin1 3-5 km

Pomenuto rudno polje o~uhva-

tastene vulkanogeno sedimeshy

ntnog porekla staropalezojshy

ske starosti duz kojih je

mestimicno javljaju proboji

plagiogranita gabrova anshy

dezita i drugih magmatskih

stena Fizicke karakteristishy

ke magmatskih stena dosta su

izmenjene (metamorfisane) a

u pojedinim delovima vulkashy

nogeno sedimentne serije zashy

uzimaju poloiaj kao tektonshy

ski uklopci eela vendsko-koshy

mbrijska serija zauzima poloshy

zaj antiklinale cija anveloshy

pa ima tendenciju neizmenicshy

nag uzdizanja i spuitanja

sa razlicitim stepenom eroshy

zije U toj strukturi smesshy

tene su brojne kvarcne fice

sa razlicitim stepenom orudshy

njenja u pogledu zlata vo1shy

frama i srebra

Stepen koncentracije kvarcnih

IIbull

Institut za bakar Bor Slika 1

L_J___