Cartier Silver Intersects 49.19 g Ag/t, 1.35% Zn and 1.31% Pb over 44.76m in Discovery Hole on the Gonalbert Property, Potosi Department, Southern Bolivia
This zone includes a higher-grade interval of 137.42 g Ag/t, 7.91% Zn and 5.6% Pb over 5.60m
Other significant intersections in the Discovery Hole include:
57.74 g Ag/t and 1.75% Pb over 18.25m including 79.90 g Ag/t and 2.53% Pb over 6.63m
109.54 g Ag/t, 3.68% Zn and 4.44% Pb over 11.09m including 170.01 g Ag/t, 2.51% Zn and 7.00% Pb over 5.81m
57.74 g Ag/t and 1.75% Pb over 18.25m including 79.90 g Ag/t and 2.53% Pb over 6.63m
109.54 g Ag/t, 3.68% Zn and 4.44% Pb over 11.09m including 170.01 g Ag/t, 2.51% Zn and 7.00% Pb over 5.81m
Channel sampling of the underground artisanal workings at Gonalbert returned the highest-grade values from the lower levels including 245.5 g Ag/t over 1.5m, 492.0 g Ag/t over 0.7m and 123.9 g Ag/t over 1.5m
Surface rock geochemical sampling has defined an extensive area of anomalous Ag and Pb extending for a strike length of approximately 2km that correlates well with the IP chargeability trends.
TORONTO, Sept. 07, 2023 (GLOBE NEWSWIRE) -- Cartier Silver Corporation (CSE: CFE) (“Cartier Silver” or the “Company”) is pleased to report the first results from diamond drilling to test geological and geophysical targets for epithermal Ag-Pb-Zn mineralization on the Gonalbert Property, Potosi Department, Southern Bolivia.
The initial program as previously reported (see Cartier Silver press release of June 29, 2023) consists of 5 drill holes totaling 3,300m collared in the general vicinity of the artisanal silver mine. To date 729.5m of drilling have been completed in two holes with a third hole in progress (Figure 1). Results have been received for drill hole DGL-01 as outlined in Table 1.
Collar locations and orientations of these holes are listed in Table 2 below.
Tom Larsen, CEO of Cartier Silver, commented: “We are very pleased with the excellent result from the inaugural diamond drill campaign at Gonalbert. Initial values from our first hole demonstrate especially solid silver grades, along with significant lead and zinc. The channel sample values from the underground workings show consistency with silver head grades reported from recent mining activity.
Regional geological and rock geochemical work on the property by our exploration team has outlined a prospective 2 kilometer long potentially silver-rich target area on Gonalbert. We are looking forward to receiving further results from this drilling program.”
Dr. Osvaldo Arce, P.Geo., General Manager of Cartier Silver’s Bolivian subsidiary, Minera Cartier S.R.L., said: “The ongoing surface and underground mapping, channel sampling and initial diamond drilling at the Gonalbert zone (southern part of the Chorrillos project), demonstrate that it is a Bolivian-type caldera hosted, polymetallic silver-dominant epithermal vein system, associated with Ordovician slates, and Miocene dacitic domes, dykes, and lithic tuffs.
Vein-type and disseminated Ag-Zn-Pb mineralization occurs in subvertically continuous fault hosted veins, and replacements of brecciated faults. The widest and highest-grade veins are present in northwest trending faults which are readily evident in the geological and geophysical data.”
Dr. Arce continued: “The Chorrillos project area occurs along a ±100 km northwest structural corridor that includes known deposits such as Chorolque (Sn), Iska Iska (Ag-Sn-Zn-Pb), Tasna (Bi-Sn-W-Au) and other large Bolivian type polymetallic deposits. It is very likely that Gonalbert may host high temperature Sn porphyry-type mineralization at depth.”
Diamond Drilling Results
The Discovery Drill Hole DGL-01, as shown in Figure 1, was drilled to test the chargeability anomaly in the Central Adit area. This hole, which was drilled at an azimuth of 60 degrees and a dip of -70E, intersected a series of high-grade epithermal silver-lead-zinc zones within a broad mineralized envelope in altered metasediments associated with steeply dipping fault zones. Significant results are as follows:
57.74 g Ag/t and 1.75% Pb over 18.25m from 115.75m to 134.00m including 79.90 g Ag/t and 2.53% Pb over 6.63m from 115.75 to 122.38m.
49.19 g Ag/t, 1.35% Zn and 1.31% Pb over 44.76m from 347.10m to 391.86m including 137.42 g Ag/t, 7.91% Zn and 5.6% Pb over 5.60m from 347.10m to 352.70m.
109.54 g Ag/t, 3.68% Zn and 4.44% Pb over 11.09m from 418.89m to 429.98m including 170.01 g Ag/t, 2.51% Zn and 7.00% Pb over 5.81m from 418.89m to 424.70m.
The true width of these intersections is approximately 80%.
Table 1: Diamond Drill Hole Assay Results as at September 7, 2023, Gonalbert Property
Hole #
From (m)
To (m)
Length (m)
Ag
Au
Zn
Pb
Cu
Sn
g/t
g/t
%
%
%
%
DGL-01
98.69
103.42
3.88
74.24
0.10
0.01
4.28
0.04
0.01
115.75
134.00
18.25
57.74
0.12
0.01
1.75
0.03
0.01
Incl
115.75
122.38
6.63
79.90
0.12
0.01
2.53
0.06
0.00
276.97
277.47
0.50
27.80
0.56
0.06
0.03
0.44
0.00
333.76
335.56
1.80
80.48
0.20
3.37
2.64
0.02
0.01
347.10
391.86
44.76
49.19
0.01
1.35
1.43
0.01
0.01
Incl
347.10
352.70
5.60
137.42
0.02
7.91
5.60
0.03
0.01
418.89
429.98
11.09
109.54
0.05
3.68
4.44
0.02
0.02
Incl
418.89
424.70
5.81
170.01
0.04
2.51
7.00
0.02
0.01
435.78
436.28
0.50
103.70
0.02
20.87
4.10
0.05
0.04
Note: True width is approximately 80% of core length. Chemical symbols: Ag = silver, Au = gold, Zn = zinc, Pb = lead, Cu = copper and Sn = tin. Quantities are given in percent (%) for Zn, Pb Cu, Sn and in grams per tonne (g/t) for Ag and Au.
Underground Channel Sampling, Gonalbert Artisanal Mine
Underground channel sampling has been carried out in the Hoyada, Labor Central Rieles (Central Adit) and Tocoyoj artisanal underground workings (Figure 1). Results (Table 3) have been received for underground sampling at Central Adit where the main production shaft is located (Figure 1). Channel sampling was systematically carried out along the ENE and NNW-oriented drifts on the principal production levels including Level 0, 100, 160 and 180.
As shown in Figure 4, apart from one sample in level 0 which returned 504.0 g Ag/t over 0.52m, the best results were obtained in the lower levels including 245.5 g Ag/t over 1.5m, 492.0 g Ag/t over 0.7m and 123.9 g Ag/t over 1.5m. Ag and Pb correlate almost perfectly in the lower levels, indicating that the silver is largely contained within galena. Galena occurs with minor pyrite and chalcopyrite, providing the chargeability target that was mapped directly in the IP/Res survey.
Geophysical data suggest that the chargeable mineralization becomes stronger with depth, reaching a maximum at the 400m limit reached with the IP/Res survey. This trend to higher Ag and Pb values at greater depth is supported by the results of sampling over four levels from the surface to -180m in the drifts at Central Adit. Drilling to date has only partially tested the extensive chargeability anomaly.
Surface Rock Geochemical Sampling
A rock geochemical surface sampling program carried out over much the Gonalbert Property, has confirmed that Ag-Pb-Zn mineralization is associated with north-northwest trending structures inferred from the IP/Res and topographic surveys (see Cartier Silver press release of June 7, 2023). Silver values show the same strong correlation with galena (Pb) that is evident in the underground workings.
The principal trend of mineralization is 310-330 degrees parallel to a set of north-northwest trending quartz dykes. The strong correlation of silver with galena indicates that the IP chargeability response from the galena (over 10% in some veins) can be used to effectively target the silver-bearing mineralization.
Figure 5 shows the distribution of Ag and Figure 6 that of Pb. Complete analytical results are given in Table 4. Samples taken are chip and channel samples.
Figure 1: Geology Plan Map of Gonalbert Property Showing Locations of Diamond Drill Holes and Artisanal Mine Workings
Figure 2: Geological Cross Section Discovery Hole DGL-01, Gonalbert
Figure 3: Chargeability Cross Section, Discovery Hole DGL-01, Gonalbert
Figure 4: Geological Cross Section showing Underground Channel Sampling, Gonalbert
Figure 5: Rock Geochemical Sampling, Gonalbert Property Showing Ag Distribution
Figure 6: Rock Geochemical Sampling, Gonalbert Property Showing Ag Distribution
Table 2: Summary of Diamond Drill Hole Coordinate in Gonalbert
Hole No.
Collar
Easting
Collar
Northing
Elev.
Azimuth
Angle
HoleLength
(m)
Holes Assays Reported
DGL-01
219000.0
7637460.0
3669.5
60°
-70°
457.0
Subtotal
457.0
Holes Assays Pending and In Progress
DGL-02
219214.7
7637583.9
3581.8
60
-70°
272.5
DGL-03
218742.2
7637542.2
3596.3
60
-50°
In progress
Subtotal
272.50
TOTAL
729.50
Table 3: Results of Underground Channel Sampling
SAMPLE #
UG LEVEL
EASTING
NORTHING
ELEV.
WIDTH (m)
STRIKE
DIP
Ag g/t
Au g/t
Pb %
Zn %
Cu %
Sn %
GLC-01
- 160
219040
7637477
3432
1.25
130
80
0.6
0.03
0.0
0.0
< 0.005
0.01
GLC-02
- 160
219023
7637474
3431
0.70
292
77
0.9
0.03
0.0
0.0
< 0.005
< 0.005
GLC-03
- 160
219003
7637493
3432
0.58
145
64
82.5
0.04
4.0
8.8
0.02
0.01
GLC-04
- 160
219004
7637496
3432
0.86
308
81
89.2
0.05
3.6
2.9
0.03
< 0.005
GLC-05
- 160
219002
7637515
3427
0.47
322
88
73.0
0.06
4.5
10.8
0.03
0.01
GLC-07
- 160
218979
7637538
3433
1.45
117
72
49.0
0.04
2.8
5.9
0.03
0.01
GLC-08
- 160
218968
7637562
3434
1.00
125
76
2.0
0.04
0.0
0.1
< 0.005
0.01
GLC-09
- 160
218952
7637594
3437
1.60
185
68
12.6
0.14
0.4
2.3
0.01
< 0.005
GLC-10
- 160
218955
7637614
3434
1.10
117
84
23.4
0.14
0.3
0.4
0.01
< 0.005
GLC-11
- 160
218909
7637675
3436
1.35
120
83
245.4
0.04
9.9
19.1
0.04
0.04
GLC-12
- 160
218887
7637703
3436
1.30
300
74
56.5
0.04
2.4
14.7
0.03
0.02
GLC-13
- 160
218878
7637711
3436
1.35
312
76
67.4
0.04
3.2
22.0
0.03
0.03
GLC-15
- 160
218852
7637755
3438
1.63
315
78
55.5
0.09
1.9
11.0
0.02
0.02
GLC-16
- 180
219032
7637476
3405
2.20
88
47
2.1
0.18
0.0
0.3
< 0.005
< 0.005
GLC-17
- 180
218992
7637513
3406
0.70
152
82
492.0
0.04
19.8
5.9
0.02
< 0.005
GLC-18
- 180
218966
7637559
3407
1.00
248
82
3.6
0.06
0.3
0.5
< 0.005
< 0.005
GLC-19
- 180
218957
7637577
3407
1.50
348
79
123.9
0.07
6.6
3.3
0.09
< 0.005
GLC-20
- 180
218895
7637684
3409
2.70
154
72
16.3
0.10
0.3
12.5
0.03
0.02
GLC-21
- 180
218921
7637666
3409
1.50
285
88
31.9
0.04
1.1
10.8
0.02
0.02
GLC-23
0
219134
7637509
3588
1.40
146
46
1.5
0.03
0.1
0.3
< 0.005
< 0.005
GLC-24
0
219102
7637495
3590
1.10
238
13
1.3
0.02
0.2
0.4
< 0.005
0.01
GLC-25
0
219096
7637492
3589
1.30
234
44
4.1
0.03
0.2
0.0
0.03
0.01
GLC-26
0
219068
7637480
3589
0.60
325
65
54.2
0.04
4.3
0.0
0.06
0.01
GLC-27
0
219063
7637478
3590
0.50
240
53
504.0
0.04
15.6
0.0
0.07
< 0.005
GLC-28
0
219013
7637457
3590
1.50
234
27
2.7
0.02
0.2
0.0
0.01
< 0.005
Table 4: Results of Surface Rock Geochemical Sampling
POINT
SAMPLE #
EASTING
NORTHING
ELEV.
WIDTH (m)
STRIKE
DIP
Ag g/t
Au g/t
Pb %
Zn %
Cu %
Sn %
SJ1
GSJ-01
219434
7636725
3613
0.40
130
75
170
0.03
7.36
0.67
0.11
0.01
SJ2
GSJ-02
219546
7637763
3622
0.39
168
82
3
0.01
0.01
0.01
0.00
0.01
SJ3
GSJ-03
219603
7637753
3613
0.23
188
79
1
0.02
0.01
0.03
0.03
0.20
SJ4
GSJ-04
219634
7637631
3591
1.60
137
60
1
0.01
0.08
0.10
0.00
0.00
SJ5
GSJ-05
219396
7637643
3599
0.40
283
50
1
0.01
0.00
0.28
0.02
0.00
SJ6
GSJ-06
219438
7637621
3585
0.70
61
58
1
0.01
0.05
0.27
0.01
0.01
SJ7
GSJ-08
219641
7637409
3557
0.30
139
80
2
1.84
0.04
0.05
0.02
0.03
SJ8
GSJ-09
219423
7637568
3587
0.36
316
83
1
0.01
0.01
0.25
0.03
0.01
SJ9
GSJ-10
219778
7637341
3507
0.64
102
63
3
0.23
0.01
0.04
0.01
0.00
SJ10
GSJ-11
218770
7638456
3590
0.35
4
66
4
0.04
0.08
0.11
0.02
0.01
GN-2
GSJ-13
218735
7637999
3575
0.38
104
80
63
0.02
3.61
0.82
0.02
0.02
GN-4
GSJ-14
218797
7637971
3593
0.40
303
85
31
0.02
0.86
1.84
0.02
0.01
G11
GSJ-15
218509
7638159
3551
0.23
308
80
4
0.07
0.06
0.01
0.00
0.01
G16
GSJ-16
218679
7638208
3571
0.24
312
84
2
0.24
0.26
0.08
0.01
0.01
G20
GSJ-17
218896
7637940
3584
0.23
116
72
123
0.04
2.24
0.20
0.02
0.02
G32
GSJ-18
219417
7636627
3626
0.36
162
81
29
0.01
0.94
0.01
0.00
0.00
G37
GSJ-19
219119
7636846
3599
0.40
336
70
39
0.19
2.60
0.03
0.02
0.01
G44
GSJ-20
219113
7637113
3629
0.50
8
66
32
0.03
1.10
0.00
0.01
0.01
G54
GSJ-22
219098
7637170
3644
0.80
175
88
21
0.03
0.28
0.01
0.00
0.02
G62
GSJ-23
219094
7637210
3651
0.10
322
70
4,160
0.27
21.00
0.01
0.01
1.65
G82
GSJ-24
219101
7637043
3626
0.20
135
78
28
0.03
0.61
0.00
0.00
0.01
G92
GSJ-25
219144
7637367
3623
0.45
172
55
31
0.02
1.50
0.01
0.04
0.02
G101
GSJ-26
219063
7637508
3639
0.80
134
70
102
0.12
5.34
0.02
0.03
0.04
G117
GSJ-28
218728
7637707
3618
0.50
140
80
1
0.02
0.03
0.01
0.01
0.00
GO10
GSJ-29
219032
7636547
3592
0.40
174
80
9
0.01
0.76
0.16
0.01
0.02
GO31
GSJ-30
219384
7637186
3549
0.25
4
85
61
0.01
1.58
0.35
0.03
0.01
GO37
GSJ-31
219606
7636797
3574
2.00
Dump sample
Dump sample
483
0.08
19.50
0.10
0.08
0.05
GO56
GSJ-33
219560
7636653
3616
0.25
178
52
23
0.01
0.30
0.00
0.01
0.00
GO66
GSJ-34
219812
7636807
3506
0.37
125
45
179
0.04
18.25
0.10
0.07
0.04
GO71
GSJ-35
219892
7636825
3474
0.70
122
68
8
0.04
0.31
0.06
0.03
0.00
GO74
GSJ-36
219843
7636733
3507
0.40
115
40
8
0.29
0.05
0.03
3.67
17.80
GO84
GSJ-37
219613
7637925
3623
4.00
12
60
4
0.06
0.10
0.02
0.03
0.02
GO90
GSJ-38
219551
7637557
3553
0.30
134
64
1
0.01
0.10
0.18
0.01
0.02
GO93
GSJ-40
219500
7637524
3536
0.12
128
82
8
0.01
0.17
0.62
0.00
0.01
GO102
GSJ-41
219311
7637635
3569
0.20
75
75
2
0.01
0.02
0.08
0.02
0.00
GO118
GSJ-42
219062
7637539
3638
2
stockwork
stockwork
5
0.09
0.38
0.00
0.01
0.02
GO120
GSJ-43
219036
7637562
3632
0.45
322
74
73
0.12
1.53
0.09
0.03
0.02
GO137
GSJ-44
219752
7636941
3474
0.2
110
65
92
0.07
3.29
0.02
0.02
0.02
G0144
GSJ-45
219572
7637030
3520
3
132
62
64
0.06
0.33
0.27
0.01
0.04
G0147
GSJ-46
219474
7637231
3524
0.18
144
86
3
0.05
0.82
0.22
0.02
0.01
GN2
GSJ-47
219797
7637258
3500
1.2
160
25
4
0.10
0.11
0.01
5.04
0.01
GO180
GSJ-51
218712
7638156
3592
0.12
285
62
5
0.60
0.14
0.15
0.05
0.00
GO205
GSJ-55
219082
7638432
3674
0.1
310
79
2
0.22
0.12
0.12
0.00
0.00
GO216
GSJ-56
219348
7637893
3595
0.1
315
77
1
0.03
0.02
0.08
0.00
0.00
GO221
GSJ-57
218815
7637502
3639
0.5
140
78
39
0.03
1.24
0.26
0.02
0.03
GG3
GSJ-72
219853
7636739
3495
0.2
135
30
7
<0.01
0.65
0.65
0.00
<0.005
G8
GSJ-73
219798
7636797
3511
0.25
170
22
153
0.05
5.16
0.08
0.14
0.02
G35
GSJ-74
219728
7636426
3601
2
Dump sample
Dump sample
345
0.03
12.70
0.28
0.03
0.35
G53
GSJ-78
219877
7636754
3497
0.2
190
15
21
0.07
2.98
0.12
0.16
0.01
G63
GSJ-80
218840
7637768
3597
0.07
93
82
44
0.21
8.52
0.06
0.07
0.02
GG4
GSJ-81
219643
7636770
3557
0.40
140
64
347
0.11
14.20
0.16
0.09
0.03
GG5
GSJ-83
219479
7636807
3590
0.35
170
41
5
<0.01
0.18
0.02
0.00
<0.005
G85
GSJ-85
219678
7636668
3563
0.15
175
37
33
0.02
0.72
0.00
0.02
0.02
GO211
GSJ-139
219390
7636837
3595
0.40
340
82
428
0.07
12.05
0.01
0.02
NA
G0212
GSJ-140
219286
7636789
3594
0.40
314
55
11
<0.01
1.02
0.01
0.00
NA
GO215
GSJ-142
219265
7636921
3594
0.30
155
55
179
0.10
0.41
0.01
0.01
NA
GO208
GSJ-143
219861
7637316
3468
0.30
114
30
75
0.05
0.03
0.03
2.82
NA
GO203
GSJ-144
219905
7637170
3433
2.00
138
32
220
0.05
0.02
0.01
0.02
NA
GO209
GSJ-145
219845
7637211
3492
0.15
190
18
2
0.01
0.02
0.01
3.17
NA
Note: NA = not analyzed
Qualified Person
Dr. Bill Pearson, P.Geo., a Qualified Person (QP) as defined under National Instrument 43-101 (NI 43-101), has reviewed and approved the scientific and technical content of this press release. Dr. Chris Hale, P.Geo., supervised the geophysical surveys. Geological surveys and diamond drill logging and sampling were supervised by Dr. Osvaldo Arce, P.Geo. Messrs Hale and Arce are QPs as defined by NI 43-101.
Rock geochemical sampling program was directed by Dr. Osvaldo Arce, P.Geo. Underground channel sampling was employed whereas for the surface rock geochemical program both channel and chip sampling method were employed.
Cartier Silver is utilizing both ALS and AHK for drill core analysis, both of whom are major international accredited laboratories. Drill samples sent to ALS are prepared in both ALS Bolivia Ltda’s preparation facility in Oruro, Bolivia and the preparation facility operated by AHK in Tupiza with pulps sent to the main ALS Global laboratory in Lima for analysis.
Cartier Silver employs an industry standard QA/QC program with standards, blanks and duplicates inserted into each batch of samples analyzed with selected check samples sent to a separate accredited laboratory.
Drill core samples sent to AHK Laboratories are prepared in a preparation facility installed and managed by AHK in Tupiza with pulps sent to the AHK laboratory in Lima, Peru. Check samples between ALS and AHK are regularly done as a QA/QC check. AHK is following the same analytical protocols used as with ALS and with the same QA/QC protocols.
About Cartier Silver Corporation
Cartier Silver is an exploration and development Company focused on discovering and developing its recently acquired silver property assets, including the Chorrillos Project and claims staked by the Company’s subsidiary, all of which are located in the Potosi Department of southern Bolivia.
The Company also holds significant iron ore resources at its Gagnon Holdings in the southern Labrador Trough region of east-central Quebec, and the Big Easy gold property in the Burin Peninsula epithermal gold belt in the Avalon Zone of eastern Newfoundland and Labrador.
For further information please visit Cartier Silver’s website at www.cartiersilvercorp.com
For further information please contact:
ThomasG.Larsen
Jorge Estepa
Chief Executive Officer
Vice-President
(800) 360-8006
(800) 360-8006
(416) 360-8006
(416) 360-8006
The CSE has not reviewed nor accepts responsibility for the adequacy or accuracy of this release.
Statements in this release that are not historical facts are “forward-looking statements”andreadersarecautionedthatanysuchstatementsarenotguaranteesoffuture performance,andthatactualdevelopmentsorresults,mayvarymateriallyfromthoseinthese “forward-lookingstatements”.
Photos accompanying this announcement are available at
https://www.globenewswire.com/NewsRoom/AttachmentNg/157827cf-eef1-4ca7-9c98-0b12a045f95d
https://www.globenewswire.com/NewsRoom/AttachmentNg/9b82d2ab-2c33-4c23-8062-bf19814816c8
https://www.globenewswire.com/NewsRoom/AttachmentNg/13ebe094-95e9-4e00-99f5-279ac96e9e13
https://www.globenewswire.com/NewsRoom/AttachmentNg/6ce602bd-92cc-413c-b3eb-e6a8f6a0e207
https://www.globenewswire.com/NewsRoom/AttachmentNg/cb1c1509-5430-4b22-aba3-08d9ca81d436
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