8/18/2019 Geologica 1991 b

1/13

UDK

55

CODEN GEOME

2

YU ISSN 0352-1206

GEOLOGIC

M CEDONIC

T.

5

1990-91-illnm-Stip

Nr. l

eo• maced. T. 5 I Nr 1 I 1 172 I SUp 1 1990 91

8/18/2019 Geologica 1991 b

2/13

I

Gcol. maeed.

T.S

Nr.l

121-132

Slip

1990-91

YJlK:553.24.065.078/497

.17

.3neToBo/1047

31/

OpHrHHaJlCH HarteH TPYJl

Original scientific: papers

XJ1WOTEPMAJ1HJI H3MEIU I BO OJlOBHO-IU1HKOBOTO

t

A.JJJlllITE

"lJIETOBO" BP3 flPHMEPOT HA PY.l(HA )K

HI.{A

nHm

T. Cepa4l

IIMOIICKR·

, Ii.

Boma,

M. MIIJlOCABJlellCKH

·

.'YAIlJlCKO.no 

IOWKII 4taKYlrnrr- lII

nm

• • P YAJUfUN OJIOIlO H QJUIK ln tTOOO

AIiCTP

AKT

X HnpOTepMaJlHHTe

HlMeHH lUI

BYJlKBHCKHTe KapnH BO on08110- mUlKOBOTO

1180taJlKW

TC 3JleTOBO H HCf'OIIaTa H C I 1 C C P J U ~ 8

OKOJ1HHB

npeTCTaBYBIlBT noce6Ho o6ejclKje H8

088

Jlyno

HOCHO

nOJlP

lI  tje.

HifTCH3HCTOT Ha aJlTCpaItHHTe

liB

RYJ1KaIICKHTe

k8pnH

( r naUHO Jle

UIt

TCKH

Hrn

HM

6pHTH) CTOJTKY CHJ1110 H3pa3eH WTO 80 neHCWHH YCJlO RH e coceM TeWKO

JlB

ce n

poIIBjJle

.

np HMepOK UB "RnOJlHO CaCJlCB upna. ElCTeH3HBHO HajpacnpOCTpaHCTa npOMella HB BYJ1IalH

CKHTe kapnH e npOnHJlHTH3aUl-tj8Ta, M3HMI\lCCTHPaH8 npeKY nojasaTa Ha XJlOPHT, nenYMJIO

enHllOT, II8Jll.lHT, nMpHT H Jlp. O n XHJlPOTCpMaJllmTe aJlTepHaUHH, tliM ,..aHHIjJeTcTaUIlH ce

KOHCT8THPBHH Hcnocpe,wIO OKOJlY py,auHTe ) (MUM, HajKB

pa

KTepHCTH'l.ItH

ce

C

HI

IHcjlHK8UHjaTB,

cepm.ltfTH33U1tjaTa i ICOMHHH38UHj aTB, npH.IlPYlKeHH OJl nHpocjJHJ1HTH38UHja, u.p60HaTHl81Ut

j a, K-cjleJmcnaTH38uHja H LIP.

n OK

paj

H3BeneHHTe T

HnH  t

HH XHJlPOTepMaJlHH HJMeHM, BO

H80tanHWTeTO

3mrrOBO ce

pernCTPHpaHH H noroneM 6poj

IIa

M TeP

RUHH

1t0H

ce UP8KTCPH3Hpa8T

co

HaMMett

ClICTCH3H

TCT HO H8MeCTB co

HBrnacell

HHTeH3HTeT. 80 ooaa rpyna Ha H3MeHH n0ce6l1o Tpe6a LIB ce

HCTaKH8T

anynaplf33UHj8n. 8prnnHT

838ulf jaTa, CHJlepKTH38UHjllTa, THTBHH3BQ)fj8TB, mtMOHH

TH3IlUHjaTB, C03JlaBBlbeTO Ha lIHJlPOMYCKOBHT, KaJlUeJ1011 H .np.

BOBE,ll

OJlOBHO-UHHKOBOTO

Hao

tammrTe 3JIeT

OBO

rH 333eMa ueHTpaJIHHTe

~ e J l O l l H ~ p

y

 

peOH

KpaTOB()-3J1eTOBO, O,llHOCHO jy roHCTOq IDlTe neno

HH Ha 3J1eTOBCKOTO PY,llHO nOJle.

llPOCTOPHO

OBa PY,llHO

Hao

r amnure e

JlOICMH3HpaHO

BO

HCTO IHHTe ,lleJlOBH

Ha

npOCTpaHaTaKpaTOBCKQ-3J1eTOBC Ka

BYJlK

aH

CKa 06J1aCT.

8/18/2019 Geologica 1991 b

3/13

122

Geologica macedonica, T .S

Nr l

1990-91

OCTaTOUHTe

o.n

cTapOTO py.napeH.e YKaX

8/18/2019 Geologica 1991 b

4/13

123

.Serafunovski, B.Boev, M.Milosavleski - Hidrotermalni...

PElYJIT TH

0 1, I1Cnl1TYBAlhATA

HcnHTYBaH>aTa H npOY'I)'BaH>aTa Ha XH,IlpOTepMaJIHHTe H3MeHH BO

HaotaJI

HlllTeTO3JIeTOBOce BprueHH Bp3 npHMepOUH O.ll aJITepHcaHlt BYJlKaR

CKH

KapnH,

3eMeHH On CaJI

6aHnHHTe neJI

ODH Ha PY

nHHTe lIGfllH

6poj

n

H III

.

np06HTe

on

PynHa

)K}fua

n

ce

3eMeHH

Ha

XOPH30HT

510

nOTKon

22,

ynpaBHo

Ha npOTeraH>eTO Ha pynHaTa

)In ua

H Ha enHaKBH paCTojaHHja JIeBO H neCHO

(CJI.

1 .

3eMeHH ce BJeTO

Ha XH,IlPOMYCKOBHT, lCa.rrn:ellOH, pOnoxp03HT H .I.l,p.

Pe3YJITaTHTe

on

R3BprneHHTe peHTreH-nHljlpaKTOMeTpHCKH HcnHTy

BaH>a nOKa)l()'B33T

HCTO

TaKa

ro

JIeM3 CJIWlHOCT. nOpanH H,IleHTH'IHOCTa Ha

peHTreH-nHljlpaKTorp aMiITe,

on BJ

8/18/2019 Geologica 1991 b

5/13

124

Geologica macedonica, T.5 Nr.l 1990-91

CJl.

1. nJlaH

H3

PY.QHa )Im

U3

6p.

I I ,

H3 XOPH30HT 510, nOTKon-22

Fig.

1.

Plan

of

ore

vein-II

of

horizons

!HO, adin-22

..

I-

=

=

: ~

-

oO

t

~

 

--

...

,  :::r.

h:=

.. .......

r -

- - - -

  ~ - - - - - - - - - - - - - - - - - - - - - -

= ~ : \

,

::..-::'

I.::

-e

'- f,'1

: : ~

.-

:-:::::;t

 .or::;

'·  1

• {§

, ..

,

..

--_._ ......

  .......

.

I t

Wk

CJJ. 2. PO ri TE! l .miC2>PAKTOrPM1

11A BY

.llI

8/18/2019 Geologica 1991 b

6/13

125

...

T .Serafimovski, B.Bocv, M.Milosavleski - Hidrotcrmalni. ..

CJI. 3. np0tl>HJlII8 py /U lil

>IU1ua

6p.

IU l1oMe -y

XOPHlOIl

T

580,

5

35

H490

Fig. 3.

Prolile for

orc vcin-lII

helwen horiz

oDS

580 535 and 490

t

••

  . U . . . L . . . . . . . . = ~

_ : . ~ _ - : : a '

5:1=

E : : I : ; r : : ; : : - . ; : : : . . ~

:

  .

8::=

4 - :

t.-

'

::=s

: M

  =

.

"S

 

.

.

.......

CJI . 4. PEIITl L:J1Jl,UIDl AKfOf PAM

llA UYJU

8/18/2019 Geologica 1991 b

7/13

Geologica macedonica,

T S

Nr.11990-91

26

TYBaHH npHMepOIJ.H ce pemcTpHpaHH

CHJIHIPHKaIJ.Hja,

Cep

HIJ.HTHJaIJ.Hja H

KOaJIHHH3aIlHja, HO, 3a paJJIHKa on

npe,axOnHHTe,

O

Bne

HMaMe HHTeHJHBHO

npojaBeHaK-IPe.rmonaTHJaIJ.Hja, 'me n

pHC

YCTBO e YTBpneHO MaJIXY nonaneJCY

on

KOHTaKTOT Ha PynHaTa )l(HlJ.a

co

OKOJIHHTe Kapm

l. nOlcpaj

OBHe

HJMeHH,

JaBH.aeH

HHTeH3lueT

nO

Ka)l(YBa H KaJIIJ.HTHJaIJ.HjaTa,

RaM

eCTa

nOJIOMHTHJa

IJ.HjaTa H

CH.aepTH

JaIlI1jaTa, a

perHCTpHpaHO

e H

npHCYCTBO Ha

nHpHT

HJaIl

H

ja

H MaHraHO-KaJIIJ.HTH.

3a na

ce

CorJIena

XeMH

JMOT

Ha

XH.apOTepMaJIHO HJMeHeTHTe BYJIKaH

·CKH

KapnH

on

HcnHT

YBaRliTe JIOKaJIHTeTH, HJpa60TeHH ce HeKOJIJCY CHJIHKaT

HH

aHaJIH3H,

a peJymaTlITe ce npmca)J(aHH BO Ta6ena 1.

TADEJIA I

XeMItCKH COCTaB H3 J M e ~ e T T e BYJlKaHCKH CTeHlt on

HenocpenHaTa OKOJlHHa Ha pynHa )l Hu.a II

HI l I

T ABLE I

Chemical composition

of

the

altered

volcanic rocks from

the

vicinity of the ore veins II and III

zr 1JI 1

ZT

lfJ2 zrn 6

ZTlf

l13

ZT

II114

zr 1111]2

ZTIIIJ23

Si02

58 .44

46.47

52 .89 52.19

54 .71

54.32 52.92

Ti02 0.83

0.

79

0.77

0.73

0.7 0.81 0.64

A120)

17.33 14.95 13 .63 15.44 14.47 15.58 13.45

Pe20)

5.25 15.28 5.31

3.67

2.59

2.46

2.75

FeO

2.ll

0.77 8.65

3.04 3.01

2.91 2.09

MnO

0.24

0.15

l.32 0.61

0.17 0.14

029

M20

1.9 1.22 2.56

2.89 2.99 2.01 1.43

Cao

1.24 1.3 0.86

5.77 6.41

6.41

9.13

Na20 0.13

0.

26

0.06

0.19

0.05

0.

89 0.25

K20

3.97

3.6

2

3.51

4.3 3.4

9 4.23

4.69

H20 0.59 0.

83 0.44

0.66

0.

38 0.39

0.26

H20

+

7.49

13.76 9.88 10.08

10.58

9.52 10.74

SUMA

99.52 99.6 99.88

99.5

7

99.55

99.

67

99 .64

On np

RJIO)l(eHaTa T

a6e

JIa

ce rJIena neKa

COCTaBOT

Ha XHnp

OTe

pMaJIHO

HJMeHeTHTe BYJIKaHCKH Kapn H O

) l

Hc nHTYBaHHOT JIOKaJIHTeT BO MHO

ry Hew

TO

ce

paJJIHKys3

on

C

OCT

aB OT Ha penaT

RBR

O CBe)l(HTe BYJIKaHCKH KapnH

on

PynHHKoT

3JIeTOBO. H

MeH

O,

on

n O,WlTou.H

Te

WTO

rH

naBaaT crOJAHOB H

PNlOBHK 1974) Ja BYJIXaHCKHTe

KapnH on

pynHH

Ko

T 3JTeTOBO MO)l(e

na ce

KOHCTaTlfpa n eXa

TIle

xapm l BO npoceK

CO

np)l(3T 58% Si0 2, OKOny 3-3,5%

K20

He

nOBeKe

on 1,5-2% H20 +.

O n

OB

a

npOHJJIerysa

n eKa

BO npOIIe

cOT

Ha

x l

t.aPoTe

pMaJI

Ha n aKTlffiROCT

nOWJIO no

HJHecYBalbe Ha Si

8/18/2019 Geologica 1991 b

8/13

127

.Serafimovski, B.Boev, M.Milosavleski - Hidrotermalni ...

CO

MaT03a Koja

ja

Cn

e.aH

CHnlf(tlHK3UHja

Ta

H HHTeH3HBHO

ce

paJBHBa

oKony

py.aHHTe )DlllH. BHCOKHOT CTeneH Ha npOMeHeTOCT Ha BynKaBCKHTe KapJIH

o.a )l(Hua n H

ce

rne.aa H o.a npoueHTyanHoTo yqeCTBO Ha

H20+

kOMnO

HeHTaTa

BO

HHBHHOT

COCTaB.

3a

.aa ce corne.aa aCOlU fjaUlIjaTa Ha

ene

MeHTHTe

BO

XH.lIpOTepManHO

H3MeHeTHTe KapnH OJl HCOHTyaaIDfoT JlOKanHTeT, H

3Bpwe

HH

ce

CeMHKBaH

THTaTHBHH CDeKTpanHH aHaml3J1

Ha HeKonxy

npHMe

p OUH o.a py.am )l(Hlla

ll.

PeJynTanrre 0 11

OBHe

HcnmyBafba

ce

Opl1.Ka)l(aHH

BO

Ta6ena

ll.

TAEEJIA

II

CeMJIKBaRTJITanmUII cnelITpaJIHlf altam!l" Ha BYJlKaUCKJITe

Kap

ml 04 PY ll lta )KJfua II

TABLE

II Semiquantitative spectral analyses

of

the volcanic

rocks from

ore

velnn

Mn

Pb

Sn

Ga Cc

Cu

Zn

A2

Co V Ni

ZTJJ/2

2000 1500

-

20 10 200 1500 3 5

7 5 3S

5

ZfD/6

2000

1500

-

20 3S

200

1500 7 5

5

35

7 5

zrW 3

2000 150

-

10

3S

20

200

5 5 50

5

ZfW14

3SOO 100

-

10

15 3S

75

5

5

S

10

ZTn/24

10000

1.50

7 5

20

10

20 500

5

-

3S

10

ZfUIl

1500 2000

-

20

7 5

150

5000

5

10

50

7 5

Zfll1l2 1500

100

2

30

10

100

-

3.5

5

50

5

ZfII/23

2000 150

-

20

15 75

35

2 5

50

5

O.a npHJlO)l(eHaTa Ta6ena ce rne.aa .aeKa YTBp.lleHaTa acoUHjaUHja Ha

eneMeHTHTe BO XH.IlpOTepManHO Jf3MeHeTHTe BynKaHcKH KapnH O.ll XOH

TaXTHHTe .aenODH DO pYAHa )l(Hlla

n

O,llf OBapa

Ha

opeonOT Ha pacejyaatbe Ha

nOJIHMeTanH lHara onOBHO-UlofHKOBHa MHHepanH3aUHja nOKanH3HpaHa

BO

PYJlHHTe

>KHUH.

HMeHo,

CO

BHCOKH

CO.llP

)I(HH ce KapaKlepH3HpaaT

onOBO

TO

,

UHHKOT, cpe6pOTO JI MaHlaHOT,

WTO

e H HopManHO 3a BaKOB

nm

Ka

Haota

JlHWTa a nOp8.llH ManaTa OCeTJIHBOCT Ha MeTO.llaTa O.llpe.neH 6poj Ha eneMeH

TH o.a pe.aOT Ha Ba, Sr, Be, Sb, Ge H.IlP. He ce perHCTpHpaHH.

.lll1CKYCHJA

Bp3

6aJa Ha

no

,aaTOUHTe O.ll,aoceraWHl-ITe

HCT

pa)l(yaafba, KaKO H

pe3yn

TaTHTe o,a Haj HoBHTe

HcnHTyaafba

Ha XH.npOTepManHHTe H3MeHH Ha

Byn

KaHCKHTe KapnK KenOcp

e.[ HO

oKony py.aHa )l(H

ua

II H

ill,

MO)l(e,aa

ce

KOHCTa

Tlipa ,aeKa

XHJlpOTepManHKTe H3MeHH BO

HaotamuDTeTO

3neTOBO

ce

.aoeTa

HHTeH311BHH H PaJHOBHJlHH,

WTO

BepojaTHo ,aoata

KaKO

pe3ynTaT O.ll COCTa

http:///reader/full/corne.aahttp:///reader/full/corne.aa

8/18/2019 Geologica 1991 b

9/13

MeTaCOMarCKa (npo.ny1IT H3 npOnl1MITCJCJiTe npOMeHH) H )l(HJ1Ha - npoJl.)'KT

Ha

Xli..llpOTepMaJIHaTa aKTHB

HOCT

• ll anery noroJ1eMO npHC

YCTBO

H 3H3'1elbe

•

Geologica macedonica, T.S Nr.1 1990-91

28

BOT

Ha CpeJlKHaTa,

Hej3HHaTIl

TeKTOHC K3 npeJlHcnOHHpaHOCT H KapaKTepOT

Ha

~ p O T e p M a n H H T e tP.nyIi..llK. KaKO eKCTeH3HB

HO

H

aj3acTa

neHa HJMeHa

Ha

BYJlKaHCKHTe KapOH BO HaOranHlllTeTO3J]eTOBO e H

npOmUllITIiJaUHjaTa

Taa

BO OCHOBa

e aBT0lrnJlpaTaUHOHa

npOMeHa Koja

HeMa JlKpeKTHa BpCRa

co

0pYJlHYBatbeTO,

HO HejJHHaTa

Y

Jlora ce

o rJleJla

BO

360raTYBstbeTO

HS PSCTBO

pHTe

CO

CYJltPYPHa H CYJltPypeCTIl KHCeJ1HHa, ICon DOBeiceKpSTHO HM ja JroJ1e

Mime arpeCHDHOCTa

Ha

Xli..llpOTepMa.IIHHTe paCTBopH. K3XO peJYJlTaT Ha

OBa,

OOJlOUHa Jloata JlO HHTeH3HDHa K-MeTaCOM8T03a H H3J1YJKYBatt.e Ha PYJlHHTe

Ko r.moaeHTH OJl

OKOJl

HHTe Kap

nH.

nponHJlH

TH3aunjaTa ce

M3HH4>ecTKpa

co

Me

TaCOMaTCKa

H3MeHa Ha

60eHHTe MHHepamt BO

BYJIKBHCKIiTe

KapnH

C03Jla

Bathe

Ha

XJlOpHT,

n   O T

ICaJIl..\HT, IDtPJlT, Ha Meers MarHeTHT H ,np.

HajUHTeH3HBHO 3aCTaneHH Xli..llPoTepMaJIHH H3MeHH BO HaotaJ

IHIllTe

TO

ce

CHJlHtPmcauHjaTa,

CepUUHTlt33IlHjaTa

H KOanl1HH3aUHjaTa

THe, BO

noro

JleMa HJlH

BO

DOMana Mepa,

ce

npojaBeHH

BO

H Ha

ICOHTIlKTOT

Ha PY. I.HHTe

)l(HUH

co

OKomuue

BYJ1KaHCKH KapnH. HHreH3HTeTOT

Ha OBHe

npO

MeHH

nOCTeneHO

on

a

ta o.nnane'lYBajKli ce

o,n PYJlHHTe

)l(I1U1-1.

B o C8Ml1Te

py,nHH

)l(HUH H BO HHBHHTe

can6aHJl

H HajHlITeH1HBHa

npOMeHa

e CHJ1HtlluKallHjaTa

Bo OJlJleJlHH JleJlOBH Taa y

8/18/2019 Geologica 1991 b

10/13

129

.Scrafimovski, B.Boev, M.Milosavleski - Hidrotermalni ...

BO HaotaJIHll1TeTO HMa

- )l(HJIHaTa

Kap60HaTH3aUHja,

Koja ce jaBYBa

KaKO

KaJI

UHTCKa, Mn-KaJIUHTCKa, Cl1l1epHTCKa HJIH aHKepHTCKa. npO

ny

KTHTe H3 Kap

60HaTH3aUHjaTa H3CT anYBaaT HJIH BO CaMocToj HH )l(HUH, )l(HJIH'-IKH H npo

)l(HJIKH Hmi

BO

3ae./lH1lua co

cllmlKHJIHaTa

Kap60Ha

T

H3anHja

BO

BHlI

Ha CHlle

p

m H 3

a

UJfja teCT

O

naTH nOKa)l(YBa H m lpeKTHa BpCKa co 0pYlIHY

BaH>

eTO, HO Haj lecTo ce M3HH

eCTHpa KaK O nOCTpYllHa

aJITepaUHj

a.

Mety '-IeCTHTe XJi l lpOTepMaJIHH

H3Memi

BO HcnHTYS8HHTe PYllHH )l(H

UH

Oll

HaotaJIHlllTeTO 3JIeTODO e H

nHpH

ciJHJIHTH3aUHjaTa.

Taa

rH

npHllp)I(ysa

OCHOBHHTe

H3Me

HH, a HaMeCTa,

KaKO

ll1TO e

cny -l

aj co CaJI6

aHllHH

Te lIen OBH

Ha PYllHa )l(Hua IT e H MOlliHe HHTeH3jiBHO 3aCTaneHa. Bo O.lU{eJIHH l leJIOBH

T33 Y'-IeCTBYBa H

co

H3.ll

30 BO

BKynHaTa Maca.

Co

nHpoHJIHTH3aUHja ce

3a

aTeHH

r .flaaHO

t

ellcnaTHTe

, H

Toa

KaKO

e

HOKpHCTaJIHTe TaKa H ¢e

l lc

na

THT

e Oll

OCHOB

Hal 3 Maca. nHpOHJ1lfT

OT

e 061('1HO

KpHD

TOKpHCTaJIecT llO

HH

03pHeCT H ce n

ojaaysa

Haj leCTo BO BliJl Ha P3.llHjaJIHO-3paKaCTH ne

ne

3aCTH

arpera

TH.

Oll XHllpOTepMaJIHHTe

H3Me

HH, KO Hll1TO BO HcnHTysaHHTe JIOKaJIHTe

TH

HaMeCTa

n   a ~ a a T Harnace

H

HHTeH

3HTeT,

noce6HO 6H

r H H3)lBOHJIe

K

eJl.llCnaTH3anHja H THTaT

HHH3

aUHjaTa.

l I H T ~ H I i B

H O

np

H

CY

CTBO Ha

K-

eJl.llCnaTH3auuj a e YTBp l leHO OKOny PYllHa )l(HUa m H

Toa He Ha

CaMJ-1

0T

KOHTa

lCT

TYKY M

anKY

nOllaJIeKY Ol l KOHTaKTOT (np0 6H

5,7 8

H IS , 16

,

17

,),

K3.lle

ll1TO

B

Y

J I K

a

H C K ~

l T

e

KapnH He

ce Tomey CHJIHO

aJITepl1pa

HH. C o OBaa H3MeHa

ce

3aaTeH

H n peTe)l(HO nJIarHOKJIaCHTe M caHH.. UIHOT.

Bo

caH }iJlHHOT T33

ce

n oj aaysa

BO

BHll Ha T31IKM )l(HJ1lf'-lKH H

npa)l(HJIK

H.

n pHCYCTBOTO H3

THTa

THHH33Ul-lja e perHCTpHpaHO

BO

C3J16aHllHHTe

lleJI

OBH Ha PYllHa

)l(IUl;a

II. HaMeC

Ta

THT

a

HH3aUHj

aTa e TOJIKY CHJIHO H3pa3eHa

ll1TO Y'-IeCTBYBa co

40-

50 BO BKYnHaTa Maca (np06a

1I 22),

a Haj"'IeCTO e

3aCTaneHa co

10-15%

BO

HCnHTysamrre n p

HMepoUH Oll

OBaa PYl lH3 )l(HUa.

KaKO pe3y

maT ua

npoj

aBeH8Ta T lU 8HH3auHja,

BO

XHllPOTepMaJIHO

H3M

eHe

THTe

Kapmf

1l0

1l1

JIO

llO

C031Iaaal-be

Ha

THTaT

HT, aHaTa3, PYTHJI, H

JlMeHHT

,

JIeYKoK

ceH

H

p.

Bo HaotaJrHUlTeTO 3JIeTOBO Oll XHllpOTepMaJIHHTe H3MeHH e perHC

TpHpaHO Yl l lTe H npH

CYCTBO

Ha 3.llYJIapH3aUH

ja,

Koja nonollP06HO e H3yqeHa

Oll CTpaH a

Ha

CTojaHoB H ~ e H K o c K H

(1974),

nOToa

Ha

ap rRnHTH331.U1j a,

aJIYHHTH

3

3UHja, 6ap

HTH3aUHja,

JIHMOHHTH3aUHj a H ,ap.,

HO

nOBeKeTo o

 a OBH

e

H3MeHH ce K3paKT epH3

Hpaa

T co Man

HH

TeH3HTeT,

llO

l leKa eKCTeH3HTeTOT

HM

e Haj -lecTo orpaHH'-IeH.

Tpe6a

l la ce HCTaKHe ,aeKa

co

cnpOBelleHHTe HcnHTysaH>a, HaKO

6ell1e

HanpaBeH

06H.Jl,

He

6eBMe

BO

MO)l(HOCT JIaTepaJIHO OKOny

PYllHHTe

)l(HUH

l la

H3.llDOHMe o,apelleHH 30HH co KapaKTepHCTH'-IHH aUHH Ha XHllpOTepMaJIHH

Te

aJITepauHH,

6HllejKH

TOKMY

BO CaJI6aHllHHTe

,aeJIOBH Ha

Py,aHHTe

)l(HUH

9 Geologica macedonica

8/18/2019 Geologica 1991 b

11/13

Geologica macedonica. T.S Nr .11990-91

30

HHTeH3HTeTOT, pa3HOBHJlHOCTa H Metyce6HoTO npeKJIOn

yaa

H.e Ha XHJlPO

TepMaJIHHTe aJITCpaUHH ce HajH3p aJeHH. CenaK, oCTaHyaa KOHcT

aTauMja

Ta

. lClC3

OKOny HCIlHTYBaHHTe PYAHH lKumt nH i l l

BO HaotamtWTcTO

3JICTOBO

1C0HTHHYHPaHO Haj3acnneHH Xl'U1p OTepMaJIHH H3Me

HH ce

CIfJIHct>HKallHja

Ta,

cePH

TH33U

Hjan

H

KOaJIHHH33uwj3Ta

O BHC XHJIpOTepMaJIH

l f

aJITepaUHH,

3ae.llH0

co

K-MeTaCOMaT03a H . leJI

O.alKRllKaT8

lCap60HaTMJauMja,

ce

CHHXpO

HH co

0PY

.llHya8

H.e

TO

H

THe

n peTc

nmya

aaT D3JKeH

npOClleKl{HCKH HHJJ.H

Ka

TOP

DO

H

aotaJIlfnITeT

O. O

Ba

e n

oce6Ho

3

Ha'fajHo a

OHHe

.aCJIODH

O. l Haota

JIlfWTeTO l iTO ce HaofaaT DO

ct>aJ

a

Ha

tlOHCTpa)l(yaaH.e.

3AKJIY1.10K

O. l

. loce

ra

H3HeceHoTo

MO)l(e . la

ce

K

OH

cTaT

H

pa

. lCKa BY JIKaHCKHTe

KapnH BO HaOraJIHWT

eT

O

3JIe

TOBO ce 3act>aTeHH co HHTeH3HBI:IH H PaJHOBHJl

HH

XHJlpOTep M

anHH

8J

IT

epauHH, ' fHH M a H H ~ T l l H H ce

H8jH

3paJeHH He-

nOcpe.llHO OK

Ony

PY.llHHTe

lKHllH

. EKCTeH3HBHO H

ajp8cnpOCTpaHeTaTa

H3Me-

Ha

Ha BYJIlC3HCKHTe KapOH e rrp OTIHJIlfTH33lJ,Hj8Ta,

Koja

BO OCHOBa npeTCTaBY

Ba aBTOJIClUlp

aT

8l{HOH3 npOM eHa co Koja ce 33ct>aTeHH 60eHHTe MHHep

anH

BO

Ka

pn

HTe. O.a XH.[lpOT

ep

MaJIHHTe H3Mel:lH Haj33CTanel:lH H HajHHTeH3HBHH

ce

ce

pHTH3a.lllfjaTa,

CHJIHct>mcallHjan H IC03.llHHHlaUWj3Ta, ICOH ce CHHXPOHH co

opY. lHyaali>eTO H npeTCT3DYBaaT 3Ha l

ajHH npocneKllHCKH

IfH.[lHKaTOpH

BO

Haota..rmWTeTO.

OBHe

H3M

eHH

pe'fHCH

pe. lOBHO

ce

npHJlPY

)l(eHH

Otl

Kap60-

H3TH38UHja, I lHpOct HJIHTH3aUl1ja H K-4>en.ncn3Tm8UHja oKpaj HHB. BO

He-

nHTyBaHHTe JI

OKaJIHTeTH e p

erHCTpHpaHO

H n pHCYCTBO Ha 3,Q}'JIapH3auHja,

THT3H1138UHja,

aprnJIlf

TH33UHja,

anyHHTH33UH

j a, JIlfMOHHTH33UHja H .D.p.,

I OH

JIOKaJIHO nOK3JKYBaaT H

a r

JIa

ceH

HH

TeH

3HTeT, HO

06H'fRO ce co

MaJI

eKCTeH3HTeT.

8/18/2019 Geologica 1991 b

12/13

131

.Serafunovski, B.Boev, M.Milosavleski - Hidrotermalni...

SUMARY

HYDROTHERMAL AL TERNAnONS IN LEAD-ZINC DEPOSIT

"ZLETOVO" ON

THE

SAMPLE ORE VEINS

n

AND I

II

T. Serafimov kJ· B, Boev· M. MDoS8vlevskJ

··

• Faculty or Geology andMlnlDg Slip

•• Lead and

ZlDc:

MInes "zIctovo"

The general characteristics

of

the volcn

ic

rocks from "Zl etovo" deposit and

its vicinity are that they are tectonically altered, strongly hydrothermally altcrized

and mineralized.

Lead and zinc mineralization is mainly located along fault structures within

the ignimbritic complex with dacitic composition. Volcanic rocks mainJy fo rmed

during oligo-miocene, but the lead-zinc mineralization, which is the product

of

the

hydrothermal activity, fo rmed during miocene.

Mineralization in Zletovo deposit was accompanied by intensive alternations

of volcanic rocks, with explicit manifetations round the ore veins.

The investigations that we have made so far have proved that in t is deposit

propylitization was the most extensive alternation in the volcanic rocks, the results

of which are seen in the occurrance

of

chlorite, epidote, calcite, pyrite etc.

During the bydrothermal activity the propylitized volcanic rocks were inten

sively hydrothermally altered so that only contours

of

previous minerals are left

behind.

Silification, sericitizati

on

and koalinization are most common hydrothermal

alterations.

Their intensity is expressed round the ore veins the most. As the contact of

the ore veins from th surrounding rocks moves away, the intensity

of

the alterations

gradualIy decreases. These alterations are simulatneous with mineralization and

they represent a significant prosperous indicator in the deposit. These typical

hydrothermal alterations in the deposit are almost accompanied by carbonatization,

pyrophylHtization and K- feldspatization (whose more intensive presence was

noticed round ore vein III.

Besides the above mentioned types of alteration, the presence

of

adularizati

on, argillitization, titanization, alunitization, limonitization, pyritization etc. have

been dctermiend. At some places occur with encreased intensity, but they generally

have

limited

extension.

8/18/2019 Geologica 1991 b

13/13

Geologica macedonica, T.5 Nr.11990-91

32

J111

TEPATYPA - REFERENCES

&J1E'll1K, H. 1983),

113BOPH

PYJlHHX KOMnOHeHTH XHJlPOTepMaJlHHX nelKHllITa (YnopcIIH8

8HaJlH3a reHeTC KHX MOJlen8 tl8 npHMepy

PYABo

r nelKH llIT8 3J1 eTOBO) . .l lOJ TO

PCK8

JlllcepnuH

j

a,

Beorp8JL

I1BAIIOB, T.

HBAII

OBA, B

,.

1974), nponHnHTH

BO

Cp Ma.cJlolntja H HHllllan

BPCK8

co

MHHepaJlH JaUHjan. VIII - JyroCnOBeHCKH

reonOlliKH

KOHrpec,

lineJl.

IV

ANOV,

T.

1977), Propylitisalion and Propylitic: Facies.

Vc

svik A, Kn . XXX VII, 135-154, Beograd.

I1BAIIOB, T .

.llElI

K OBCKI1

t 1980),

XH

JlPOTCPMIlJ1illt

arrrepaUHH

BO

nop lHpcKOTO

63KaPHO

nelKHllITe nnaBHU8 - 3naTHU8 BO KpaTOBclto -

3nC

TOBCK8n

BynK8t1cK8

06nacT.

CHMn03HjYM

AnTepHauHja

CTeHa

H

MHHepaJl

8 ,

139-163, BeOrp8Jl.

PAKI1K, C. 1978), HCKe

CTpYKTY

pe H retl

eTCKe oco6eHO CTH nOnHM

eTaJlH'iKOr 0pYJlHC\-ha y

3neTOBJlCKOM PYJltlOM nO

Jb

Y. IX KOHrpec reonora Jyrocn8BHjc, 611-619, CapajeB

o.

PA.llOBI1K, H. 198

1), n pOJlYKTH H8 xHJlPoTepManHHTe H

lMCIIH.

Bo

MHHepaJlOlllKO-neTpOnOlllK8 CTYJlHj8 H8

KapnHTe

OJl Jlymt8THHHTe 80 nOlUHpOKaTa

OKonHlla

HS

.l l06pe

ocKOTO

PYJlHO

H80taJ1HllITe. CTp. tjJOllll

HS

PYJl)IHKOT

3

ner

OBO

.

crOJAHOB, P .l lflIKOBCKI1,

t  

1974),

MHllepaJ101llKO-neT

pOrpstl>cKa

cTY

AHja Ha lK

Hua 6p.

2 .llo6peBo. CTp.

tjJO

HJl H8 PYJlJIKKOT 3neTOBo.

CTOJAIIO

B, P.

PA

.llODI1K

,

H. 1974),

neTp

onorHja Ha

By

nu

cKHTe u pn

BO

onoBo-UHnK08

HOT

PY

JlIIHK

.ll06peno. VITI- j

yrocnoBCHCKH

reonOWXH 1t0Hrpec, line

Jl.

CTOJAHO

B,

P.

1

980)

, BynK8HCKa

Ta

ltyn8 nnaBHU8,

nOmUCCTaJlHHTe MH llepaJ111

3

3UHH

H

oKon YPYJlHHTe n

pOM eH

H

BO HC

a. CHMn03H jyr.t

"Am

epH8lI,J1j8

CTeHa

H

MHII P B J I a ~

122-139, 1ie0rp8JL

CTOJAHO

B, P. CEPAH

MOnCKI1

, T. 1990), B

ynKaHH3MOT

BO

3n

eTOBCKO-

xpaTo

BcK8T8

BynJ:BHCK

8 06nac

T.

XJI-jyrocnoBCHcllH reon

OlliKH

KOHrpeC,

OXPHJl.

CEPAI1MOBC

KH

, T . 1

990).

M en.norcHltj8

H8

]OH8Ta J1cue-Xa.n

KH

JlHK .lloXTOPCKa

IDIcepT8UHja, IIlTHn.

t p t

EIlI1K, B. t OPtEnI1K, n . 1982),XHnpOTepMaJllle

H3Melle

Y3JIeTOBCKOM

PYIltiOM

nOJbY.

Bo CTYIlHjRT& PernOtlaJIH8 H IleT8Jbtl8 MeT

aJ10

reTCKa HCTp. YPYJlIIOM nOJbY 3neTOBo .