geologica 1991 b
TRANSCRIPT
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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
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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
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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
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zr 1111]2
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Si02
58 .44
46.47
52 .89 52.19
54 .71
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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.
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3.97
3.6
2
3.51
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9 4.23
4.69
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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.
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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
-
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200
1500 7 5
5
35
7 5
zrW 3
2000 150
-
10
3S
20
200
5 5 50
5
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15 3S
75
5
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S
10
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10000
1.50
7 5
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10
20 500
5
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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
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9 Geologica macedonica
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Geologica macedonica. T.S Nr .11990-91
30
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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.
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32
J111
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