ALPHAMIN ANNOUNCES SUCCESSFUL INFILL DRILLING AT MPAMA

Grand Baie, Mauritius , Feb. 10, 2023 (GLOBE NEWSWIRE) -- Alphamin Resources Corp. (AFM:TSXV, APH:JSE AltX, “Alphamin” or the “Company”), a producer of 4% of the world’s mined tin1 from its high-grade operation in the Democratic Republic of Congo, is pleased to announce completion of the infill drilling campaign at Mpama South and an updated Mineral Resource Estimate (MRE) for Mpama South.

HIGHLIGHTS

  • Substantially improved the confidence of Mineral Resources at Mpama South whilst extending the known mineralisation boundary.
  • Increased Indicated Resources by 286% to 3.26Mt based on assays from 63 additional infill and extensional drillholes.
  • Mpama South Mineral Resources now stand at:
    • 3.26Mt @ 2.46% Sn for 80.2kt contained tin in the Indicated category; and
  • 2.84Mt @ 2.42% Sn for 68.7kt contained tin in the Inferred category.
  • Significant additional resource growth potential at Mpama South as the deposit still remains open down-dip.
  • Mpama South Mine construction works progressing according to plan – project completion expected to increase Alphamin’s annual contained tin production from the current 12,000tpa to ~20,000tpa, approximating 6.6% of the world’s mined tin1.

Mpama South Updated Mineral Resource Estimate

In just 24 months, Alphamin has:

  • delivered a top-10 globally significant CRIRSCO compliant tin deposit by contained tin1 at Mpama South;
  • grown the resources to ~2.2 times versus the Maiden Mineral Resources and PEA2 numbers;
  • increased resource confidence across the deposit; and
  • commenced mine construction through own cashflows.

This brings forward an additional planned ~7,200tpa contained tin production, which will make Alphamin one of the largest tin producers globally and delivers on the Company strategy of organic growth and creating shareholder value.

The updated Mineral Resource for Mpama South follows eight months after the previous update announced on 31 May 2022. The update is based on receipt of assays for another 63 infill and extensional drillholes completed subsequent to the previous estimate which was based on 124 drillholes. The updated Mineral Resource is presented in Figure 1 along with the direction in which mineralisation is still open down dip and significant high grade periphery drilling intercepts.

The updated MRE now includes results from 187 drillholes at Mpama South as well as 6 drillholes drilled in 2015 in the area between Mpama South and the Mpama North ore body. The MRE was estimated using the Canadian Institute of Mining, Metallurgy and Petroleum (CIM) Best Practice Guidelines (2019) and is reported in accordance with the 2014 CIM Definition Standards.

Figure 1: Updated Mpama South Mineral Resource 07 February 2023 with selected intercepts and direction in which mineralisation is still open
[img]http://www.globenewswire.com/api/ImageRender/DownloadFile?resourceId=5e942198-2885-4d1e-97eb-68aedc255a5b&size=3[/img]
Source: Alphamin 2022

The Mineral Resource is classified into the Indicated and Inferred categories and is reported at a base case tin cut-off grade of 1.0%, which satisfies reasonable prospects for economic extraction. Mpama South Indicated Resources increased by ~286% to 3.26Mt by converting Inferred Resources, while Inferred Resources grew nominally by ~275kt (excluding those tonnes converted to Indicated). The Mineral Resource Estimate, which is effective as of 07 February 2023, is presented in Table 1 below:

Table 1: Updated Mpama South Mineral Resources effective date 07 February 2023

ClassificationTonnes (millions)Sn %Sn Tonnes
(thousands)
Indicated33.262.4680.2
Inferred42.842.4268.7

Mineral Resources that are not Mineral Reserves do not have a demonstrated economic viability and require advanced studies and economic analysis to prove their viability for extraction.

Extensional drilling down-dip and in the shallower northern and southern portions of Mpama South can be conducted at the Company’s election to carry on extending known mineralisation at Mpama South, which is still open in multiple directions. High grade drillholes around the peripheries where mineralisation remains open are highlighted in Figure 1, showing the remaining prospectivity for Resource expansion. However, for 2023, the focus will primarily be aimed at the Mpama South Mine construction and commissioning efforts, while exploration drilling will be curtailed, instead, focusing on further field work campaigns to support future programs.

The MRE has been completed by Mr. J.C. Witley (BSc Hons, MSc (Eng.)) who is a geologist with 34 years’ experience in base and precious metals exploration and mining as well as Mineral Resource evaluation and reporting. He is a Principal Resource Consultant for The MSA Group (an independent consulting company), is registered with the South African Council for Natural Scientific Professions (SACNASP) and is a Fellow of the Geological Society of South Africa (GSSA). Mr. Witley has the appropriate relevant qualifications and experience to be considered a “Qualified Person” for the style and type of mineralisation and activity being undertaken as defined in National Instrument 43-101 Standards of Disclosure of Mineral Projects.

Bisie Ridge Regional Exploration Update

Alphamin intensified exploration drilling on the 13km long Bisie Ridge from Q3 2022 to test highly anomalous soil, geophysical and structural targets identified during 2021. 8,773 metres of the 10,000 metre Phase 1 diamond core programme have been completed along the Ridge, with the remainder due for completion in Q1 2023.

Although anomalous mineralisation has been confirmed in drilling on the Ridge, it is not of the obvious coarse visual cassiterite type frequently seen in drillcore from Mpama North and South.

Only ~25% of assays have been returned from the independent laboratory to date from the Ridge drilling. Assay results when received will support a fuller investigation into the regional setting, along with data from the on-going geophysical downhole surveys, structural investigations and mapping, thereby enabling a refocused exploration programme. Until then, the key focus at site remains the construction and commissioning of the new Mpama South Mine.

Qualified Persons

Mr Jeremy Witley, Pr. Sci. Nat., B.Sc. (Hons.) Mining Geology, M.Sc. (Eng.), is a qualified person (QP) as defined in National Instrument 43-101 and has reviewed and approved the scientific and technical information contained in this news release. He is a Principal Mineral Resource Consultant of The MSA Group (Pty.) Ltd., an independent technical consultant to the Company.

____________________________________________________________________________

FOR MORE INFORMATION, PLEASE CONTACT:

Maritz Smith                                
CEO                        
Alphamin Resources Corp.                        
Tel: +230 269 4166
E-mail: msmith@alphaminresources.com
____________________________________________________________________________

CAUTION REGARDING FORWARD LOOKING STATEMENTS

Information in this news release that is not a statement of historical fact constitutes forward-looking information. Forward-looking statements contained herein include, without limitation, statements relating to the anticipated future exploration and resource estimation activities and outcomes and the timing thereof and expected increases in tin production from the development of the Mpama South deposit and the cost and timing of such development activities. Forward-looking statements are based on assumptions management believes to be reasonable at the time such statements are made. There can be no assurance that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements. Although Alphamin has attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking statements, there may be other factors that cause results not to be as anticipated, estimated or intended. Factors that may cause actual results to differ materially from expected results described in forward-looking statements include, but are not limited to: uncertainty of future exploration and assay results and consistency with past results and expectations; uncertainties related to the technical and economic parameters applied in the Mpama South Preliminary Economic Assessment regarding forecasted tin prices, the tin grade mined and processing recoveries as well as operating costs; uncertainties inherent in estimates of Mineral Resources, global geopolitical and economic uncertainties, volatility of metal prices, uncertainties with respect to social, community and environmental impacts, uninterrupted access to required infrastructure, adverse political events, impacts of the global Covid-19 pandemic as well as those risk factors set out in the Company’s Management Discussion and Analysis and other disclosure documents available under the Company’s profile at www.sedar.com. Forward-looking statements contained herein are made as of the date of this news release and Alphamin disclaims any obligation to update any forward-looking statements, whether as a result of new information, future events or results or otherwise, except as required by applicable securities laws.

Neither the TSX Venture Exchange nor its regulation services provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this news release.

Appendix 1: SAMPLE PREPARATION, ANALYSES AND QUALITY CONTROL AND QUALITY ASSURANCE (QAQC)

For sample preparation, analyses and quality control and quality assurance, see the Company’s news release dated 07 March 2022 entitled “ALPHAMIN ANNOUNCES MAIDEN MINERAL RESOURCE ESTIMATE AND POSITIVE PRELIMINARY ECONOMIC ASSESSMENT FOR MPAMA SOUTH”

Appendix 2: SIGNIFICANT INTERCEPTS (0.5% Sn lower threshold)

Hole

EastingNorthing RLm

Azi (°)

Dip (°)

From

To

Sn %

WidthSample Position
GPSGPS(m)1mid_xmid_ymid_z
BGH017582535988482273255-10237.8238.84.991.00582,7329,884,966678.6
BGH018

582535

9884822

732

93

0

141.2144.42.073.15582,6919,884,820727.9
145.8151.00.765.25582,6969,884,820727.9
BGH019582535988482273285-5147.0152.02.055.00582,6969,884,837715.8
BGH020

582535

9884822

732

84

-15

160.6164.41.453.80582,7049,884,846689.3
169.3171.15.421.80582,7119,884,846687.7
BGH021

582535

9884822

732

93

-15

109.2110.33.201.10582,6549,884,821700.1
164.6167.33.292.72582,7089,884,818687.6
BGH022
582554
9884785
732
90
0
75.080.53.995.53582,6339,884,784729.3
109.0110.01.351.00582,6649,884,785729.9
119.2122.12.222.88582,6769,884,785730.1
BGH023

582535

9884822

732

75

-15

171.4174.31.722.89582,7109,884,859683.7
175.9178.01.092.15582,7149,884,860683.0
BGH024

582554

9884785

732

103

-5

127.7129.60.541.90582,6799,884,749717.2
138.0142.01.134.05582,6909,884,746716.2
BGH025
582535
9884822
732
55
-20
212.3213.40.601.15582,7249,884,919662.3
218.0221.52.293.45582,7319,884,921660.7
222.7223.713.051.00582,7349,884,923659.9
228.0234.82.736.80582,7419,884,926658.0
BGH026
582554
9884785
732
113
-10
103.7108.03.304.29582,6499,884,735713.7
134.8136.53.721.65582,6769,884,722708.6
161.0162.55.611.50582,6999,884,711704.5
BGH030
582554
9884785
732
115
-20
110.0111.47.241.40582,6559,884,753692.2
141.9152.54.8510.60582,6869,884,745680.0
158.0161.23.613.20582,6999,884,742675.3
174.5175.811.031.35582,7139,884,738670.5
BGH032
582554
9884785
732
125
-20
177.0178.71.701.72582,6929,884,684671.3
182.0188.33.006.25582,6979,884,679669.1
190.3193.00.952.75582,7029,884,676667.2
194.4202.01.377.60582,7079,884,672665.3
203.5208.02.674.50582,7139,884,668663.2
BGH034
582554
9884785
732
115
-25
174.8178.011.993.20582,6899,884,696653.3
195.7200.01.214.30582,7069,884,686644.8
202.4206.71.864.28582,7119,884,683642.3
208.0213.31.405.30582,7169,884,680640.1
216.3221.31.425.05582,7229,884,676637.3
225.7231.00.705.35582,7309,884,671634.0
BGH027
582544
9884822
732
68
-27
212.4214.00.581.65582,7299,884,879634.0
226.0229.31.323.30582,7419,884,883628.4
235.5236.61.541.13582,7499,884,885625.2
BGH028
582554
9884785
732
90
-10
125.0126.01.721.00582,6769,884,772700.9
136.1137.21.851.08582,6879,884,770698.4
140.3142.01.031.72582,6919,884,770697.4
147.5151.32.883.79582,6999,884,769695.5
BGH029
582544
9884822
732
93
-25
126.0128.44.662.35582,6639,884,826678.5
178.9184.11.255.15582,7139,884,827657.7
193.7196.13.952.35582,7269,884,827653.0
BGH031

582544

9884822

732

75

-25

208.0211.50.993.53582,7299,884,876639.9
219.4222.41.162.98582,7399,884,879636.0
BGH033

582544

9884822

732

60

-27

259.0265.57.326.46582,7569,884,929612.8
268.5270.51.021.99582,7629,884,931610.0
BGH035
582554
9884785
732
90
-25
152.0165.02.9613.00582,6869,884,816665.0
171.0173.61.472.60582,7039,884,815657.4
176.6180.12.403.48582,7099,884,814654.9
BGH036

582544

9884822

732

65

0

147.5151.42.313.90582,6879,884,878724.8
156.6160.70.934.02582,6969,884,881724.7
BGH037
582554
9884785
732
105
-30
154.0157.03.813.00582,6809,884,741647.5
194.6197.61.542.95582,7129,884,730626.0
208.0211.21.293.23582,7239,884,726619.3
216.3220.22.793.90582,7309,884,723615.1
222.4226.71.774.30582,7359,884,721612.1
BGH038
582544
9884822
732
75
-30
151.7154.65.222.90582,6779,884,851654.3
218.3223.73.385.35582,7359,884,861621.4
226.7231.51.954.80582,7439,884,862617.6
BGH039
582554
9884785
732
100
-22
112.1113.02.120.92  582,6659,884,755687.6
116.3121.03.334.65582,6619,884,753686.1
145.0166.02.2021.00582,6969,884,744674.2
174.5176.00.951.50582,7139,884,739668.9
BGH040

582544

9884822

732

60

-30

232.0233.00.951.00582,7259,884,922618.2
273.7277.13.793.35582,7619,884,937600.0
BGH041582500988484773255-25340.0344.53.034.50582,8079,885,002599.5
BGH042
582544
9884822
732
60
-35
277.4280.01.932.65582,7519,884,922569.4
308.5312.00.623.50582,7769,884,932552.6
313.0315.61.522.55582,7799,884,933550.5
BGH043
582544
9884822
732
100
-10
102.5104.22.691.65582,6449,884,808709.0
123.0124.01.061.00582,6639,884,805704.8
163.6167.02.823.36582,7049,884,798696.7
BGH044582500988484771070-35330.0334.11.314.13582,7649,884,941533.4
BGH045
582544
9884822
732
100
-20
120.7121.831.551.10582,6569,884,806687.4
156.0159.40.563.40582,6899,884,799674.7
176.7183.63.246.92582,7089,884,795668.1
BGH046
582544
9884822
732
100
-30
195.2206.02.8510.82582,7129,884,795630.5
212.5215.21.902.65582,7239,884,793623.7
218.0220.67.162.60582,7289,884,792620.8
225.0226.04.361.00582,7339,884,791617.7
BGH047

582565

9884535

718

60

0

121.6124.60.912.99582,6539,884,879739.2
147.1148.11.281.00582,6759,884,889741.1
BGH048

582567

9884509

727

90

0

140.8143.10.902.30582,7089,884,496727.7
146.5148.00.741.47582,7139,884,495728.0
BGH049582565988453571865-15145.4147.44.272.00582,6899,884,599674.5
BGH0505825679884509727105-5160.0161.41.061.38582,7229,884,469711.7
BGH051
582565
9884535
718
40
0
134.8137.02.232.20582,6629,884,630712.3
151.0156.31.205.30582,6759,884,642711.4
164.2169.53.955.27582,6859,884,651710.8
171.3172.64.081.30582,6889,884,655710.6
BGH05258256798845097271200205.9207.11.861.20582,7329,884,385722.9
BGH053
582565
9884535
718
40
-15
173.7176.99.583.20582,6859,884,653669.2
178.6181.44.072.88582,6889,884,656667.9
192.4196.93.284.45582,6989,884,666664.0
198.9206.82.457.91582,7049,884,671661.8
207.5209.55.041.97582,7089,884,675660.3
214.7216.02.321.35582,7139,884,680658.6
BGH054No significant intercepts
BGH055582565988453571880-15145.0146.00.621.00582,7059,884,549682.7
BGH056No significant intercepts
BGH057No significant intercepts
BGH058582565988451072795-5153.4155.61.982.25582,7179,884,501703.9
BGH0595825679884536718950165.0166.03.631.00582,7329,884,528714.4
BGH060No significant intercepts
BGH0615825679884536727130-10157.6159.21.221.62582,7199,884,525677.7
BGH062582567988453771895-15154.0156.02.182.00582,6959,884,589650.2
BGH063
582782
9884646
829
270
-70
186.3194.40.828.12582,7199,884,661650.5
197.4202.51.125.03582,7159,884,661641.8
205.0209.10.834.05582,7129,884,661635.4
211.1218.92.067.77582,7099,884,661628.3
220.4222.60.862.15582,7069,884,661622.5
231.0233.00.872.00582,7019,884,661613.0
BGH0645828889884976839270-50220.8222.60.631.80582,7469,884,976668.9
BGH065

582913

9885057

819

270

-60

271.0276.02.934.95582,7699,885,057586.1
291.6292.61.701.00582,7599,885,057570.9
BGH066

582888

9884976

839

270

-60

276.0278.68.492.59582,7549,884,965596.1
300.0301.01.781.00582,7429,884,965576.6
BGH067
582913
9885057
819
270
-67
295.8300.53.214.72582,7899,885,065548.1
303.0304.61.561.62582,7869,885,065543.1
337.0338.00.551.00582,7699,885,068514.3
BGH068

582913

9885057

819

270

-50

247.0248.22.101.20582,7499,885,051633.1
251.8255.11.753.30582,7459,885,051628.8
BGH0695828889884976839270-70321.8324.73.842.93582,7799,884,962534.7
BGH0705829139885057819270-73331.0336.43.005.35582,8029,885,040505.2
BGH071No significant intercepts
BGH072

582852

9884845

831

270

-67

274.6279.72.705.10582,7499,884,847574.0
290.4294.83.614.40582,7429,884,847560.0
BGH0735827319884691838280-60121.0123.00.722.00582,6719,884,702731.9
BGH074
582944
9885130
798
270
-67
278.9283.92.855.03582,8109,885,137551.2
285.5289.11.603.61582,8079,885,138546.3
294.5297.37.142.79582,8029,885,139539.1
299.7303.30.533.69582,7999,885,139534.5
BGH075
582731
9884691
838
270
-70
115.4116.76.761.25582,6909,884,690729.4
119.5120.815.221.30582,6889,884,690725.7
125.1129.83.564.71582,6849,884,690719.3
162.6164.68.942.08582,6679,884,689687.8
BGH076
582752
9884801
849
300  
-40
108.0109.00.841.00582,6829,884,844779.6
118.8119.53.710.65582,6759,884,848772.7
128.2131.02.822.85582,6689,884,852765.8
136.7137.00.970.30582,6639,884,855761.0
BGH077
582944
9885130
798
270
-72
316.8321.22.574.36582,8309,885,130501.7
323.0328.42.565.36582,8279,885,130495.8
329.1330.10.521.07582,8259,885,130492.4
335.3337.49.632.11582,8229,885,130486.5
339.8340.17.070.30582,8209,885,131483.4
BGH078
582752
9884801
849
280 
-40
102.0106.01.884.00582,6749,884,816782.6
108.0109.00.621.00582,6719,884,817779.7
115.0117.20.802.15582,6659,884,818774.8
BGH079
582852
9884845
831
270 
-73
290.2294.41.004.25582,7659,884,842552.6
296.3302.39.466.00582,7639,884,841546.1
304.8305.718.750.89582,7619,884,841540.5
312.0313.01.081.00582,7589,884,841533.8
316.9321.64.654.73582,7559,884,840527.5
322.6328.05.415.43582,7539,884,840522.0
329.0329.51.590.53582,7519,884,840518.4
340.7341.44.290.74582,7479,884,839507.6
BGH080
582944
9885130
798
270
-75
339.9343.61.053.70582,8539,885,141469.2
345.0346.64.111.55582,8519,885,141465.5
360.7361.011.950.30582,8469,885,143451.5
BGH081a

583022

9885299

776

270

-50

269.0274.61.995.56582,8389,885,306578.6
275.6275.90.640.30582,8359,885,307576.0
BGH082a
583013
9885209
752
270
-50
263.8266.33.432.47582,8369,885,222556.0
268.4269.23.320.80582,8339,885,223553.5
277.0277.315.650.30582,8279,885,224547.9
BGH083No significant intercepts
BGH084

583023

9885299

776

270

-57

279.0280.96.251.95582,8579,885,307552.8
283.1286.31.283.25582,8549,885,307549.2
BGH0855830239885299776270-65294.7298.40.833.70582,8909,885,304512.9
BGH086

583013

9885208

752

270

-57

275.4280.83.075.43582,8479,885,214530.1
286.1286.518.900.46582,8419,885,215524.4
BGH0875830239885299777270-75263.8264.30.590.53582,9469,885,305525.0
BGH088
583012
9885208
752
270
-67
297.7299.511.931.72582,8769,885,221487.3
301.0301.86.790.77582,8759,885,221485.0
303.7304.02.470.30582,8739,885,222483.0
305.7306.01.660.30582,8729,885,222481.4
307.2307.66.660.35582,8719,885,223480.2
308.3308.912.150.67582,8719,885,223479.2
309.5309.81.980.31582,8709,885,223478.3
310.4310.717.650.33582,8699,885,223477.6
313.0313.92.820.85582,8689,885,224475.3
324.5324.95.770.38582,8619,885,226466.3
325.4325.810.400.40582,8619,885,226465.6
BGH089
582951
9885352
779
270
-50
198.0199.04.581.00582,8229,885,357628.9
202.7203.512.250.80582,8199,885,357625.5
205.1205.57.960.44582,8189,885,357623.7
217.5218.531.901.00582,8099,885,358614.1
BGH090
582951
9885423
769
270
-50
168.8170.52.451.68582,8439,885,424638.3
170.9171.512.550.60582,8429,885,424637.1
173.0173.35.050.33582,8419,885,424635.6
BGH0915829519885352779270-65222.1223.54.021.40582,8509,885,358581.3
BGH0925830219885430752270-55193.5193.917.150.38582,9139,885,431591.9
BGH093
583013
9885345
759
270
-70
224.3224.84.060.50582,9329,885,341549.9
225.8226.71.810.92582,9319,885,341548.3
227.7228.32.750.60582,9309,885,341546.7
BGH094
582990
9885055
810
270
-65
381.0384.83.843.81582,8089,885,054473.5
389.7390.35.950.51582,8059,885,054467.4
408.5411.05.822.55582,7959,885,054450.4
BGH095
582960
9884759
831
270
-60
391.6399.64.568.03582,7739,884,762482.7
400.0401.01.851.00582,7709,884,761478.6
405.0412.04.476.97582,7669,884,761471.9
414.0414.31.360.30582,7639,884,761467.2
BGH096No significant intercepts
BGH097

583013

9885345

759

270

-58

242.0245.51.103.50582,8799,885,344555.7
247.0250.12.663.10582,8769,885,344551.8
BGH099No significant intercepts
BGH100

583013

9885345

759

270

-79

226.8231.32.094.51582,9659,885,347535.2
233.1235.01.581.92582,9649,885,347530.3
BGH101
582990
9884975
813
270
-65
387.4388.62.661.25582,8029,884,968474.7
392.3394.71.492.35582,7999,884,968470.1
396.0398.20.532.24582,7979,884,968467.1
402.7410.23.687.46582,7929,884,967459.3
423.6425.513.481.84582,7819,884,967444.5
BGH102No significant intercepts
BGH103
582951
9885423
767
270
-64
161.9167.01.715.17582,8829,885,425618.5
167.8172.11.114.29582,8809,885,425613.4
173.4177.01.713.65582,8779,885,425608.7
BGH104
582985
9885054
811
270
-72
459.4463.010.193.65582,8299,885,047378.1
464.8465.18.350.30582,8279,885,047374.8
471.4475.51.724.15582,8239,885,046367.3
477.6478.00.960.42582,8219,885,046363.5
485.9486.22.120.37582,8179,885,045356.3
BGH105
582963
9884842
834
270
-70
406.5407.00.980.48582,8079,884,837458.9
410.2413.01.202.80582,8059,884,836454.6
416.9421.41.664.45582,8029,884,836447.9
421.8425.04.333.21582,8009,884,836444.1
427.7431.30.803.55582,7979,884,836438.7
434.6437.41.112.77582,7949,884,835433.0
442.3442.61.980.30582,7919,884,835427.3
446.0446.31.240.30582,7899,884,834424.1
453.7454.00.620.30582,7859,884,834417.4
457.8459.95.032.17582,7839,884,833413.0
461.7462.60.910.93582,7819,884,833410.2
BGH106No significant intercepts
BGH1075829919884982814270-75496.9502.28.215.21582,8269,884,984343.4
BGH108
582963
9884905
828
270
-62
377.2377.511.950.31582,7869,884,895495.2
381.5381.87.400.30582,7849,884,895491.5
385.3387.54.502.20582,7819,884,895487.6
391.0395.02.093.96582,7779,884,894482.1
401.0402.01.441.00582,7739,884,894475.1
405.3409.42.404.05582,7699,884,893470.3
BGH109No significant intercepts
BGH110
582963
9884905
828
270
-73
459.2467.41.008.14582,7999,884,879397.0
468.1476.710.358.58582,7959,884,878389.2
485.5486.210.300.70582,7889,884,876377.8
489.8490.92.011.12582,7869,884,875374.0
BGH111
582959
9884759
831
270
-55
334.4341.34.246.89582,7689,884,745553.1
342.4350.04.927.65582,7629,884,745547.0
352.5357.30.674.75582,7569,884,744540.6
358.3361.30.633.03582,7539,884,744537.0
362.7367.20.584.50582,7499,884,744533.3
368.0370.23.152.16582,7469,884,743530.4
BGH112

582870

9885354

790

270

-55

130.3130.62.320.30582,7979,885,360681.8
135.3135.75.690.44582,7949,885,360677.7
BGH113

582910

9885205

780

270

-62

213.0216.60.943.60582,8109,885,204590.1
229.0230.04.491.00582,8039,885,204577.3
BGH114
582870
9885354
790
270
-63
138.5138.94.400.36582,8079,885,358666.2
143.3143.66.840.30582,8059,885,358662.1
147.0147.63.830.65582,8039,885,358658.8
151.5151.80.820.30582,8019,885,358655.0
BGH115No significant intercepts
BGH116

582886

9884671

818

270

-58

285.4292.03.516.63582,7279,884,661577.7
292.5294.01.041.54582,7249,884,660574.2
BGH117No significant intercepts
BGH118

582842

9885430

769

270

-60

95.095.92.050.90582,7959,885,430686.6
100.6100.90.950.30582,7929,885,430682.1
BGH1195828429885430769270-75103.0105.02.332.00582,8149,885,431669.5
BGH120

582886

9884671

818

270

-70

323.0327.40.984.41582,7469,884,662528.2
330.3334.41.924.14582,7419,884,662522.6
BGH121No significant intercepts
BGH122
582853
9885112
780
275
-65
153.4157.51.504.09582,7869,885,123640.6
158.1161.91.263.81582,7849,885,123636.5
162.8165.01.662.25582,7839,885,123633.1
BGH123

582960

9884759

831

270

-70

432.0437.11.965.05582,7899,884,746432.8
438.5438.81.200.30582,7879,884,746429.3
BGH124No significant intercepts
BGH125No significant intercepts
BGH126b

582842

9885204

800

270

-65

150.8151.61.260.76582,7859,885,211659.7
164.0164.31.230.3582,7809,885,212647.8
BGH127

582854

9885112

781

275

-50

145.0145.31.440.3582,7609,885,121669.8
155.3158.00.622.75582,7539,885,121661.1
BGH128
583076
9885130
758
270
-68
400.8407.34.476.51582,9049,885,137393.4
408.8410.40.721.55582,9019,885,138388.9
412.6416.01.113.4582,8999,885,138385.1
BGH129

582912

9885391

786

270

-60

175.6178.51.642.93582,8269,885,391631.3
181.1181.40.950.3582,8249,885,391627.6
BGH130
582824
9885062
788
265
-50
126.3127.01.330.68582,7409,885,062693.0
133.0134.00.911582,7369,885,062687.9
139.2139.65.430.4582,7329,885,062683.5
BGH131

582931

9885285

801

270

-53

196.9200.60.713.7582,8059,885,289647.4
210.0210.30.90.3582,7979,885,289638.9
BGH132

582912

9885391

786

270

-50

169.0172.71.463.74582,8069,885,388652.1
175.8176.21.60.4582,8029,885,388648.1
BGH133

582851

9885511

764

270

-60

49.650.32.540.68582,8259,885,513720.8
53.653.82.380.22582,8239,885,514717.5
BGH134No significant intercepts
BGH135
582836
9885387
775
270
-50
82.082.90.630.89582,7859,885,387710
92.793.01.440.3582,7789,885,387702
104.0105.00.671582,7719,885,387693
BGH136
582852
9885467
759
270
-58
65.166.01.320.86582,8179,885,467704
69.872.30.692.55582,8159,885,467699
75.779.113.41582,8119,885,467694
BGH1375829319885285801270-62224.4230.61.416.2582,8309,885,285598
BGH1385828369885387775270-6597.497.72.30.3582,7959,885,387687
BGH1395829519885468748270-59123.9127.60.983.77582,8869,885,472641
BGH1405829879885256783270-50249.5253.61.264.05582,8319,885,266586
BGH1415829129885164783270-50174.6179.31.294.72582,8029,885,170645
BGH142

582912

9885016

826

270

-50

230.4235.81.295.39582,7669,885,018645
236.7238.31.981.58582,7639,885,018641
BGH143

582912

9885164

783

270

-60

210.8215.80.865.04582,8039,885,172600
225.3225.72.060.35582,7969,885,173590
BGH144a

582987

9885255

783

270

-60

264.6266.82.171.85582,8579,885,263552
269.1269.40.33.1582,8559,885,264549
BGH145
582912
9885016
826
270
-60
265.5271.02.595.48582,7869,885,013589
271.4272.81.171.37582,7849,885,013586
282.2282.516.250.3582,7799,885,013577
BGH146No significant intercepts
BGH147No significant intercepts
BGH148No significant intercepts
BGH149
582954
9884799
834
270
-55
335.4337.22.11.75582,7619,884,799559
342.0346.04.454582,7579,884,799553
347.7350.72.433.07582,7549,884,799548
352.3352.85.120.51582,7529,884,799546
362.5363.00.570.5582,7469,884,799537
BGH150No significant intercepts
BGH151No significant intercepts
BGH152D1

582821

9884623

805

269

-72

257.0259.92.012.85582,7319,884,621564
263.0263.39.060.3582,7299,884,621559
BGH153
582953
9884875
834
270
-55
327.5330.61.63.14582,7669,884,880563
333.4336.52.623.06582,7639,884,880559
342.4345.71.633.29582,7579,884,881551
347.0349.70.572.68582,7559,884,881548
367.8368.74.40.91582,7439,884,881532
BGH154No significant intercepts
BGH155No significant intercepts
BGH156

582988

9885258

789

270

-68

289.2289.82.570.65582,8759,885,264523
296.6296.90.770.3582,8729,885,265516
BGH157No significant intercepts
BGH158
582802
9885086
788
270
-47
105.4107.20.681.75582,7409,885,087701
113.0117.00.854582,7359,885,087694
120.0120.80.610.75582,7329,885,087690
BGH159
582975
9884940
822
270
-72
436.4437.73.661.33582,8199,884,932415
448.0449.00.621582,8149,884,932405
457.2457.61.280.4582,8109,884,933397
BGH160
582903
9885087
806
270
-50
219.1219.51.120.38582,7559,885,090645
221.6222.01.290.49582,7539,885,090643
226.7230.00.743.3582,7499,885,090638
233.6233.92.710.25582,7459,885,090635
BGH161No significant intercepts
BGH1625828519885512764270-7459.059.66.570.56582,8359,885,512707
BGH163
583009
9885093
799
270
-70
409.7417.13.377.36582,8689,885,098411
420.7422.10.551.42582,8659,885,098403
423.8429.00.745.24582,8639,885,099399
429.6429.91.960.3582,8629,885,099396
432.0433.00.591582,8609,885,099393
BGH164

582776

9884574

797

270

-70

171.0172.00.721582,7099,884,571639
176.0180.00.764582,7079,884,570633
BGH165

582903

9885087

806

270

-60

242.9247.22.414.27582,7719,885,083600
248.4250.02.141.61582,7699,885,083597
BGH166
582823
9884623
806
270
-60
208.9209.71.060.75582,7209,884,623623
214.2218.10.523.9582,7179,884,623618
221.0222.32.961.26582,7149,884,623613
BGH1675829759885388767270-53195.7200.51.854.86582,8569,885,388609
BGH168

582982

9885169

770

270

-50

252.6257.31.934.69582,8329,885,192565
263.4263.619.40.25582,8279,885,193558
BGH169a5828239884616794270-79301.0301.81.060.75582,7459,884,613503
BGH170
583009
9885093
799
270
-60
365.0370.12.55.1582,8309,885,095478
371.9376.02.164.15582,8279,885,095473
376.9377.13.940.25582,8259,885,095470
388.9390.01.131.1582,8199,885,096459
BGH171
582982
9885169
770
270
-62
275.5278.01.42.52582,8479,885,185529
285.5289.40.633.9582,8419,885,186520
291.9292.216.50.3582,8389,885,187517
BGH172No significant intercepts
BGH173
582982
9885167
766
270
-70
319.6322.45.182.8582,8739,885,176464
325.7330.04.664.28582,8719,885,177458
330.9336.62.245.69582,8699,885,177452
BGH1745830109885093799270-50363.5366.00.812.5582,7919,885,091507
BGH175
582976
9885388
767
270
-71
187.8192.32.154.5582,9169,885,392587
193.9197.33.333.4582,9149,885,392582
199.4199.90.610.55582,9139,885,392578
203.7204.82.361.12582,9129,885,392573
BGH176
582993
9884984
814
270
-78
512.7516.21.13.46582,8499,884,970321
518.0522.32.444.25582,8479,884,970315
525.5528.01.642.55582,8459,884,969309
BGH177
582958
9884766
831
253
-63
405.6409.21.093.56582,7749,884,706473
412.6414.91.792.32582,7719,884,705467
421.4421.74.390.24582,7679,884,704461
BGH178No significant intercepts
BGH1795829599884769831248-70489.6491.21.111.6582,7989,884,701373
BGH180b
582774
9884571
794
270
-77
213.1215.90.912.85582,7229,884,571582
217.5222.61.585.11582,7209,884,571576
224.1224.30.890.25582,7199,884,571573
BGH181
582955
9884806
837
270
-63
369.5372.51.413.02582,7789,884,809511
377.3379.58.382.21582,7749,884,809505
385.4385.71.20.3582,7709,884,809499
BGH182
582953
9884875
835
270
-65
393.0395.24.082.22582,7949,884,872474
403.4408.24.664.81582,7899,884,872464
416.2416.50.630.34582,7859,884,872454
424.9425.51.830.61582,7819,884,872446
439.5439.724.60.25582,7759,884,872433
446.8449.00.952.17582,7719,884,872426
BGH183
582844
9884709
843
270
-71
285.7289.00.833.33582,7499,884,711572
290.0293.52.693.54582,7479,884,711568
296.0296.71.080.7582,7469,884,711564
299.3303.44.674.14582,7449,884,711559
305.5306.15.890.65582,7429,884,711555
309.8313.22.993.44582,7409,884,711550
314.1318.01.523.9582,7389,884,711546
322.0323.90.861.86582,7369,884,711539
BGH184
582957
9884767
834
270
-52
321.4324.92.13.42582,7589,884,761579
327.3329.15.91.87582,7559,884,760575
331.5333.53.082.05582,7529,884,760572
337.0339.00.672582,7489,884,760568
340.6342.50.531.96582,7469,884,759565
345.6350.010.664.4582,7429,884,759561
352.0355.80.573.8582,7389,884,758556
356.5356.71.960.24582,7369,884,758554
BGH185
582849
9884706
842
270
-75
326.4331.81.955.31582,7609,884,706525
332.8335.61.992.83582,7589,884,706521
339.7342.00.732.3582,7569,884,706514
345.1345.41.660.26582,7549,884,706510
BGH186
582953
9884802
834
270
-71
410.9423.53.9412.58582,7999,884,799447
424.0427.00.613582,7959,884,799440
433.4435.52.752.1582,7919,884,799432
441.1448.54.847.35582,7869,884,798423
449.0452.43.43.35582,7849,884,798417
BGH187
582991
9884982
814
278
-61
365.7368.41.652.73582,8089,885,001496
372.5373.010.51582,8059,885,001491
375.6376.00.750.45582,8049,885,002489
381.9385.47.443.5582,8009,885,002482
387.9391.02.43.12582,7979,885,002477
394.2394.52.380.25582,7949,885,002473
409.6410.025.30.4582,7869,885,003460
BGH1885829919884982814284-67Independent assays still outstanding

Appendix 3: Checklist of Assessment and Reporting Criteria

Drilling techniquesAll drillholes were diamond drill cored and drilled from surface (most intersections drilled using NQ size), holes drilled orientated in an east-west direction were angled between -60° and -70°. Holes collared in the west were drilled out in fan patterns into the side of a hill and angled between 0° and minus 35°.
LoggingAll of the drillholes were geologically logged by qualified geologists. The logging is of an appropriate standard for grade estimation.
Drill sample recoveryCore recovery in the mineralised zones was observed to be very good and is on average 97%.
Sampling methodsHalf core samples were collected continuously through the mineralised zones after being cut longitudinally in half using a diamond saw. Drillhole samples were taken at nominal 1 m intervals, which were adjusted to smaller intervals in order to target the cassiterite vein zones. Lithological contacts were honoured during the sampling. MSA’s observations indicated that the routine sampling was performed to a reasonable standard and is suitable for evaluation purposes.
Quality of assay data and laboratory testsAt the on-site ABM laboratory (managed by Anchem), samples were first checked off against the submission list supplied and then weighed and oven dried for 2 hours at 105 degrees Celsius. The dried samples were crushed by jaw crusher to 75% passing 2mm, from which a 250g riffle split was taken. This 250g split was pulverised in ring mills to 90% passing 75μm from which a sample for analysis was taken. Samples were homogenised using a corner-to-corner methodology and two samples were taken from each pulp, one of 10g for on-site laboratory assaying and another 150g sample for export and independent accredited 3rd party laboratory assaying.

Received samples at ALS Johannesburg are checked off against the list of samples supplied and logged in the system. Quality Control is performed by way of sieve tests every 50 samples and should a sample fail, the preceding 50 samples are ground in a ring mill pulveriser using a carbon steel ring set to 85 % passing 75μm. Samples are analysed for tin using method code ME-XRF05 conducted on a pressed pellet with 10% precision and an upper limit of 5,000ppm. The over-limit tin samples are analysed as fused disks according to method ME-XRF15c, which makes use of pre-oxidation and decomposition by fusion with 12:22 lithium borate flux containing 20% Sodium Nitrate as an oxidizing agent, with an upper detection limit of 79% Sn.

Prior to the 2021 drilling the assays were also conducted at ALS Global in Johannesburg where samples were analysed for tin using fused disc ME-XRF05 with 10% precision and an upper limit of 10 000 ppm. This was reduced to 5,000 ppm from 2014 onwards. Over limit samples were sent to Vancouver for ME-XRF10 which uses a Lithium Borate 50:50 flux with an upper detection limit of 60% and precision of 5%.
ME-ICP61, HF, HNO3, HCL04 and HCL leach with ICP-AES finish was used for 33 elements including base metals. ME-OG62, a four-acid digestion, was used on high grade samples for Pb, Zn, Cu & Ag.
External quality assurance of the laboratory assays for the Alphamin samples was monitored. Blank samples (299), certified reference materials (434) and duplicate samples (357) were inserted with the field samples accounting for approximately 11% of the total sample set.

The QAQC measures used by Alphamin revealed the following:
  • Blank samples indicated that no significant contamination occurred overall. Low levels of contamination (mostly <200 ppm Sn) mostly occurred, however 12 values between 229 ppm and 1,285 ppm were returned. Given the high grades at Bisie, the levels of contamination are not significant.
  • Five different CRMs were used with expected values between 0.18% and 31.42% Sn. The lower grade CRMs were prepared by Ore Research and Exploration (OREAS) and the two high grade CRMs (4.19% and 31.42% Sn) by the Bureau of Analysed Samples Ltd (BCS). In general, ALS returned values within the tolerance limits (three standard deviations) for the OREAS CRMs, although slightly lower than the expected values. Assays of the highest grade BCS CRM were mostly outside of the three standard deviation limits but within ±4%of the expected value. The update assays of the high grade BCS-355 CRM were within ±2% of the expected value with an overall low bias relative to the CRM expected value. For the 5.07% Sn BCS CRM, assays were consistently lower than the expected value by as much as 7%. This trend continued for the update assays with an average under-assay of 5% relative to the CRM expected value. Overall, the CRMs results indicate a slight negative bias for the ALS assays.
  • Coarse duplicates show mostly excellent correlation, indicating minimal error in the process and a high degree of repeatability.
Verification of sampling and assayingThe mineralisation in thirteen of the drillholes completed in 2021 at Mpama South were visually verified during a site-visits by the QP in August 2021 and several of the initial drillholes were examined during earlier site visits to Bisie. The QP observed the mineralisation in the cores and compared it with the assay results. It was found that the assays generally agreed with the observations made on the core. Core photos from the drilling programme have regularly been provided to the QP for inspection.

105 pulp duplicates were sent to SGS (Johannesburg) in November 2021 for confirmation assaying.
  • The pulp duplicates showed acceptable correlation with the ALS assays at both high- and low-grade ranges with an overall bias of near zero.
    • Average bias for grade ranges > 1% is less than 1%.
    • Tendency for ALS to be higher (~5%) for the grade ranges less than 1%.
  • Inter-lab precision (after removal of <0.10%) is 85% within 10% error and 95% within 20% error
Location of data pointsThe drillhole collar positions were surveyed using a differential GPS.

Downhole surveys were completed using a multishot down-hole survey instrument (Reflex EZ-Track), or north seeking gyro (Reflex EZ-Gyro / Reflex Gyro Sprint-IQ).
Tonnage factors (in situ bulk densities)Relative density measurements were made on the majority of recent drillhole samples using the Archimedes Principle of weight n air versus weight in water. A regression formula of tin grade against relative density was developed and applied to the samples that did not have direct measurements. The assigned specific gravity was interpolated into the block model using ordinary kriging.
Data density and distributionA total of 124 holes were drilled in Mpama South. An additional 6 holes previously drilled in the Wedge area of Mpama North have been included in the Mineral Resource. Holes were drilled steeply from east to west, along section lines spaced approximately 60 m to 80 m apart. Several sets of holes were drilled in a fan pattern into the side of a steep hill, with orientations spanning from the northeast to the southeast (from azimuth 045° to 125°). These drillholes fans intersect the mineralisation 25 m to 40 m apart in most of the Mineral Resource area.
Database integrityData was provided as Excel files. MSA completed spot checks on the database and is confident that the Alphamin database is an accurate representation of the original data collected.
DimensionsThe mineralisation consists of seven zones, with a total extent of 950 m along strike. MZ1 has a strike length of 950 m and 500 m down-dip and MZ2 has a strike length of 650 m and 500 m down-dip. Together, these two zones account for 88% of the Mineral Resource. The zones occurring in the footwall and hangingwall of the MZ1 and MZ2 tend to be narrower and irregular in shape with strike lengths from 100 m to 300 m. MZ6, which is located to the south has a strike length of 270 m and a dip length of 110 m.
Geological interpretationThe mineralised intersections are clearly discernible in drill core. The Mineral Resource is interpreted to occur as irregular veins and disseminations of cassiterite that when combined form tabular mineralised zones, dipping 65-70° to the east. The mineralised zones are hosted in chlorite schist that is the result of intense hydrothermal alteration associated with a fracture system.

MZ1 is the largest zone by volume of the Mineral Resource, with an extent of 950 m and an average thickness of 4.1 m. MZ2 is the second largest zone, with a strike length of 650 m and an average thickness of 3.4 m. However, the thicknesses of these two zones vary from as little as 1 m, up to 13 m thick.

Three smaller zones (MZ3 to MZ5) occur in the footwall of the main zones of mineralisation which progressively become narrower, moving away from the main zones. MZ3 thickness ranges from 1 m to 9 m with an average thickness of 1.5 m. MZ4 has an average thickness of 1 m, attaining a maximum thickness of 5 m. MZ5 has an average thickness of 1.2 m, ranging from 1 m to 5 m. All zones become narrower along the edges, where they pinch-out.

A narrow zone (MZ7) occurs in the hangingwall of the main mineralisation with an average thickness of 0.5 m and a maximum thickness of 4 m.

MZ6, which occurs to the south, tends to be lower in grade and has an average thickness of 4 m, ranging from 1 m up to 9 m. MZ6 is not part of the Mineral Resource.
A three-dimensional wireframe model was created for the seven zones of mineralisation based on a grade threshold of 0.40% Sn. MZ1 and MZ2 make up the main zone, which are the most consistent zones and occur within a persistent chlorite schist. Narrower less continuous zones occur above and below the main zone within chlorite-mica schists.
DomainsThe mineralisation was modelled as seven tabular zones containing irregular vein style mineralisation. A hard boundary was used to select data for estimation in order to honour the sharp nature of vein boundaries.
CompositingSample lengths were composited to 1 m by length and density weighting.
Statistics and variographyStatistics for the seven estimation domains show distributions that are positively skewed with coefficients of variation (CV) ranging from 1.3 to 1.96, the only exception being domain MZ7 which shows lower variability due to very few composites resulting in a CV of 0.79.

The two main zones (MZ1 and MZ2) have similar average tin grades (2.22% and 2.11% respectively). The smaller, footwall zones (MZ3 to MZ5) are higher in tin grade with averages ranging from 3% to 4.41% while MZ6 and MZ7 are lower in tin grade, with an average of 0.63% and 1.07% respectively.

Normal Scores semivariograms were calculated in the plane of the mineralisation, down-hole and across strike. Variograms were modelled for tin, with a range of 40 m within the plane of mineralisation and with a range of 3 m across the structures.
Top or bottom cuts for gradesTop caps were applied to outlier values, identified as breaks in the cumulative, probability plots.
Data clusteringData clustering occurs where the fan drilling, collared on the western side of the deposit, intersect the surface drilling collared in the east, resulting in a data spacing of 25 m to 40 m towards the centre of the deposit. Outside of this area, the grid spacing becomes more regular, 60m to 80 m along strike and 50 m down-dip.
Block sizeA rotated block model with a parent cell of 10 mX by 10 mY by 2 mZ was used. Sub-celling was used to divide the parent cells to a minimum sub-cell of 1 mX by 1mY by 0.2 mZ to closely fit the narrow portions of the vein structures
Grade estimationTin, copper, lead, zinc, silver, arsenic and density were estimated using ordinary kriging. A minimum number of 5 and a maximum of 10 one metre composites were required for the tin and density estimates. A minimum of 5 and maximum of 8 composites were used for the other elements.
Estimation was carried out in three passes, with the first pass using search volumes coinciding with the variogram ranges. A second pass estimate expanded the search volumes by a factor of 1.5 to estimate blocks where insufficient samples were present for an estimate in the first pass. Where blocks remained un-estimated from the first two passes, a third pass, using an expansion factor of 10 was used to ensure all blocks in the model received a grade and density estimate.

Dynamic Anisotropy was used to orientate the search volumes to the strike and dip of the individual mineralised zones.
Resource classificationIndicated Mineral Resources were declared where the drillhole spacing is approximately 40 m and where the geological model has low variability. The remainder of the interpreted model was classified as Inferred Mineral Resources, corresponding to areas informed by drilling spaced 50 m to 80 m apart with a maximum extrapolation of 20 m from the nearest drillhole.
Mining cuts and cut-off grade assumptions.A minimum of 1 m was applied to the mineralisation model. The thickness, grade and steep dip implies that the Mineral Resource can be extracted using established underground mining methods similar to those applied at Mpama North.

A 1% cut-off grade was applied based on the Mpama North costs and prevailing tin price.

Isolated blocks above cut-off grade in dominantly low-grade areas of the model were not included in the Mineral Resource
Metallurgical factors or assumptionsThe tin mineralisation occurs as cassiterite, an oxide of tin (SnO2). At Mpama North gravity separation is used to produce a tin concentrate. The Cu, Zn and Pb mineralisation occurs as sulphides, which are removed by flotation to create the cassiterite product. It is assumed that similar processes will be used to process the Mpama South mineralisation.
Legal aspects and tenureAlphamin through its wholly owned DRC subsidiary, Alphamin Mining Bisie SA, has a Mining License PE 13155 which includes the Bisie Tin Mine. Alphamin has an 84.14 percent interest in ABM. The Government of the Democratic Republic of Congo (GDRC) has a non-dilutive, 5% share in ABM.
Audits, reviews and site inspectionThe following review work was completed by MSA:
  • Inspection of approximately 20% of mineralised core intersections used in the Maiden Mineral Resource estimate.
  • Database checks.
  • Inspection of Mpama South drill sites in August 2021.
  • On-site review of the exploration processes.
  • Laboratory inspections.


1 Based on data obtained from International Tin Association Tin Industry Review 2022
2 See News Announcement 7 March 2022 for Preliminary Economic Assessment and Resources
3 CIM Definition: An Indicated Mineral Resource is that part of a Mineral Resource for which quantity, grade or quality, densities, shape and physical characteristics are estimated with sufficient confidence to allow the application of Modifying Factors insufficient detail to support mine planning and evaluation of the economic viability of the deposit.
4 CIM Definition: An Inferred Mineral Resource is that part of a Mineral Resource for which quantity and grade or quality are estimated on the basis of limited geological evidence and sampling. Geological evidence is sufficient to imply but not verify geological and grade or quality continuity.


ALPHAMIN ANNOUNCES SUCCESSFUL INFILL DRILLING AT MPAMA