Hole 23FP006 includes 65 metres at 1.9 g/t gold and including 10 metres at 3.0 g/t gold

  • Hole 23FP006, a scissor hole that cuts across discovery hole 23FP002, confirms the lateral continuity of gold mineralization for about 180 metres in a northeast direction and starting at a drill hole depth of 31 metres.
  • The vertical extent of gold mineralization at the Fazenda do Posto discovery has been traced for 330 metres.
  • Vertical Hole 23FP003 drilled 58 metres grading 1.0 g/t gold starting at a drillhole depth of 80 metres within a larger gold mineralized interval of 214 metres.

TORONTO, Nov. 27, 2023 (GLOBE NEWSWIRE) -- Lavras Gold Corp. (TSX-V: LGC, OTCQX: LGCFF) reports that follow up drilling at the Fazenda do Posto discovery on the Company’s LDS Project in southern Brazil has validated the discovery reported in August 2023 (Lavras Gold press release August 29, 2023). The discovery has been confirmed in terms of gold grades, widths and continuity and remains open in several directions to resource expansion.

The highlight in this press release is scissor hole 23FP006 which returned assay results with continuous mineralization of 230 metres grading 0.9 g/t gold starting at 31 metres and including:

  • 204 metres grading 1.0 g/t gold from 31 metres including:
    • 65 metres grading 1.9 g/t gold from 149 metres; and including
    • 10 metres grading 3.0 g/t gold from 154 metres.

The Fazenda do Posto discovery is located roughly 150 metres west of the Lavras Gold Butiá Gold Deposit, which has an NI 43-101 gold resource (* footnote below) of approximately 500,000 ounces and is open to expansion.

Drill hole 23FP006, reported in this press release, tested the northeastern extension of Fazenda do Posto and was drilled southwest on a 200-degree azimuth and a dip of 060 degrees. The hole was collared approximately 210 metres northeast of 23FP002 – the discovery hole announced on August 29, 2023. Continuous gold mineralization was encountered in 23FP006 starting at a drill hole depth of 31 metres (vertical depth of about 27 metres) for 230 metres. Table 1 tabulates the metre-by-metre assay results.

“We are very pleased to validate the Fazenda do Posto gold discovery with this scissor hole, which cross cuts the earlier hole that returned 340 m at 1.1 g/t gold,” commented Lavras Gold President & CEO Michael Durose. “While it is still early in the drilling program, we are delighted to have intercepted another very long and continuous zone of gold mineralization starting at a shallow depth and running for over 200 metres. This is a unique bulk tonnage near-surface gold system characterized by remarkably continuous gold mineralization within an episyenite host rock. A higher-grade core of gold mineralization is beginning to develop based on the limited drilling we have completed so far. Drilling is ongoing and we look forward to additional drill results as we begin to unravel this new gold discovery.”

This discovery at Fazenda do Posto is ideally located adjacent to the 500,000 ounce Butiá gold deposit that outcrops at surface, pointing to the development of a critical mass of gold mineralization in this area. These new results continue to move Lavras Gold closer to its objective of developing an economically feasible bulk tonnage open pit gold mine.

Despite record rainfalls in the region that have hampered access to drilling sites and caused delays in the drilling program, the Lavras team is fast-tracking the process of defining the geometry and grade distribution of this important new discovery. Two drill rigs are working in this target area and have completed over 3,000 metres of drilling in 14 holes since making the discovery at Fazenda do Posto. Assay results will be released in meaningful batches following interpretation.

[* Footnote: Butiá hosts an NI 43-101 compliant near-surface gold resource of about 500,000 ounces, as detailed in the NI 43-101 Technical Report Mineral Resource for Butiá Gold Prospect dated and effective January 25, 2022. The report was prepared by VMG Consultoria e Soluções Ltda. for Lavras Gold Corp. and is available on the Company’s website and www.sedar.com under Lavras Gold’s issuer profile.]

Discussion of drilling results

The Fazenda do Posto discovery is located along the western edge of the Lavras do Sul intrusive complex approximately 4.7 kilometres southwest of the town of Lavras do Sul (Figure 1). The discovery is in an area of recessive topography about 150 metres west of the Butiá Gold Deposit.

Follow-up Drilling Confirms Discovery at Fazenda do Posto

Assay results have been received for four drill holes that drilled a total of 1,520 metres at the Fazenda do Posto discovery. A summary of these results is shown in Table 2. This also includes results from hole 23FP002 – the discovery hole that was released on August 29, 2023.

A plan (aerial) view showing the location of all drill holes is shown in Figure 2. A cross-section facing west is shown in Figure 3.

Key highlights are as follows:

  • Three drill holes – FP002, FP003 and FP006 have returned significant gold assay results displaying continuous gold mineralization over very long intervals. The gold mineralization typically occurs within a brick-red coloured episyenite. The gold is usually associated with fine grained disseminated pyrite and/or arsenian pyrite and usually occurs with iron-rich dark green to black chlorite. Grey-white carbonate vesicles are typically associated with the gold mineralized zone. Photos showing examples of mineralized episyenite are shown in Figure 4, Figure 5 and Figure 6.
  • Gold mineralization has been traced over a northeast-southwest extent of about 180 metres, and a vertical distance of 330 metres. Gold mineralization starts at a vertical depth of about 26 metres in the northeast area, as defined by drill hole 23FP006, and approximately 100 metres depth as defined by drill hole 23FP002.
  • A higher-grade core of mineralization appears to be developing in the centre of the deposit, flanked by lower to moderate gold grades along the margins.

Highlights of drilling are detailed below and summarized in Table 2.

Drillhole 23FP001 was collared along the southeast edge of Fazenda do Posto with a drill hole azimuth of north 020 degrees and dip of 60 degrees. The hole returned narrow modest gold values and is interpreted to be on the eastern edge of the mineralized block of Fazenda do Posto close to a northeast trending fault. This hole was drilled primarily in perthitic granite, with a minor interval of mineralized episyenite. The hole appears to have stopped short of the main episyenite target interpreted to occur to the northeast of the end of the hole.

Drill hole 23FP002 (previously released discovery hole) was collared in the southwestern portion of the target area with an azimuth of north 020 and an inclined angle of 60 degrees. The highlights of drill hole 23FP002 are 340 metres grading 1.1 g/t gold from 117 metres including:

  • 160 metres grading 1.8 g/t gold from 199 metres including
    • 27 metres grading 2.1 g/t gold from 208 metres
    • 68 metres grading 2.1 g/t gold from 293 metres

This hole confirms gold mineralization to a vertical depth of about 390 metres.

Further details of this hole can be found in the Lavras Gold press release dated August 29, 2023.

Drillhole 23FP003 was collared 95 metres northeast of 23FP002 and drilled vertically. The hole encountered albitized Fazenda do Posto granodiorite and then intersected a lamprophyre dike at 3 metres. This was followed by altered granodiorite and then a small interval of mineralized episyenite at 24 metres. This was followed by another interval of altered granodiorite until about 87.0 metres. Strongly mineralized episyenite was encountered at a drillhole depth of 87.0 metres (75 metres vertical depth) continuously with intervals of mineralized perthitic granite to a depth of 294 metres (see Figure 4). Highlights of gold mineralization include:

  • 214 metres grading 0.50 g/t gold from 87 metres including
    • 140 metres grading 0.7 g/t gold from 87 metres including
      • 58 metres grading 1.0 g/t gold from 87 metres including
        • 39 metres grading 1.2 g/t gold from 106 metres

Significantly, when intervals of less than 0.25 g/t gold within the mineralized envelope are removed, the remaining mineralized interval of hole 23FP003 returns 0.9 g/t gold over 105 meters.

23FP004 was collared 130 metres northwest of 23FP002. The hole missed the target as the azimuth of the hole was oriented 200 degrees and pointed away from the target. However, hydrothermal alteration in the form of albite and chlorite was observed throughout the hole suggesting the rocks have good potential for finding mineralization at depth.

23FP006 was collared 210 metres northeast of 23FP002. This hole is a scissor hole that was drilled southwest on a 200-degree azimuth and a dip of 60 degrees. The purpose of the hole was to determine the depth and continuity of gold mineralization along the northeastern portion of the target above the trace of hole 23FP002. As highlighted in the cross section in Figure 3, the zone of gold mineralization starts at 31 metres down the drillhole (about 27 metres vertically below surface). Significant hydrothermal alteration in the form of albite alteration occurs within cover rock above the zone of gold mineralization.

The hole returned assay results with continuous mineralization of 230 metres grading 0.9 g/t gold starting at 31 metres and including:

  • 204 metres grading 1.0 g/t gold from 31 metres including:
    • 65 metres grading 1.9 g/t gold from 149 metres; and including
      • 10 metres grading 3.0 g/t gold from 154 metres.

Significantly, when intervals of less than 0.25 g/t gold within the mineralized envelope are removed, the remaining mineralized interval of hole 23FP006 returns 1.2 g/t gold over 162.9 meters.

Table 1 tabulates the assay results for the mineralized interval of drill hole 23FP006. Sampling was completed on 1 metre intervals for the entire length of the drill hole. Three 50 gram aliquots were assayed for each 1 metre sample, and the average grade of the three aliquots was used to derive the final gold grade.

Next steps at Fazenda do Posto and Butiá

Indications are that a significant gold mineral system is developing at the Fazenda do Posto gold discovery and the adjacent Butiá Gold Deposit.

Two drill rigs are on site testing these areas.

One near-term objective is to define the geometry and gold grade distribution of the Fazenda do Posto discovery and look for more blind discoveries. A second near-term objective is to test for extensions to the mineralized footprint of the Butiá Gold Deposit.

The medium-term goal is to de-risk the Fazenda do Posto discovery and Butiá Gold Deposit such that a preliminary economic study defining the general scope of a gold mining project can be prepared.

Regional exploration is on-going, with the goal of defining new exploration targets on the very prospective 22,000-hectare LDS Project.

OVERALL LDS EXPLORATION PROGRAM MARKED BY EXCEPTIONAL SUCCESS

In addition to these positive developments, Lavras Gold has had exceptional exploration success since going public in April 2022. A regional drone magnetic survey has been completed, and regional soil geochemistry programs are on-going. The Caneleira Gold Discovery has been reinterpreted, and new gold mineral systems have been found at Zeca Souza, Galvao, Matilde, Matilde Extension, and Vila Marieta. Although Butiá and Fazendo do Posto are developing into the centre of gravity at LDS, the exploration upside on the property is very significant and on-going strategies are in place to continue exploring for and testing new targets.

Qualified person

Michael Durose, Lavras Gold’s President and CEO, is a qualified person as defined by NI 43-101. He has reviewed and approved the scientific and technical information contained in this release.

Quality assurance and quality control

For the Fazenda do Posto discovery, sample handling, preparation, and analysis are monitored through the implementation of formal chain-of-custody procedures and quality assurance/quality control programs designed to follow industry best practices.

All drill hole samples in this drilling program consist of split NQ diamond drill core.

Drill core is logged and sampled in a secure facility located in Lavras do Sul, Rio Grande do Sul State, Brazil. Drill core samples for gold assay are cut in half using a diamond saw and submitted to ALS Laboratories Inc. in Goiania, Goiás State, Brazil for preparation by crushing to 85% passing 1.0 mm, riffle splitting to obtain 500 g aliquots, and pulverizing to 85% passing 75 microns.

Pulps are shipped to ALS Laboratories Inc. in Lima, Peru and analyzed by a 50g fire assay and AAS finish. Three 50g aliquots are taken for samples in the mineralized zone and one aliquot is taken in fresh rocks. The average grade of the three aliquots is used to determine the final grade of the mineralized sample.

Certified standards, non-certified blanks and field duplicates are inserted into the sample    stream at regular intervals, so that QA/QC accounted for about 10% of the total samples. Results are routinely evaluated for accuracy, precision, and contamination.

Lavras Gold has been targeting larger intersections of greater than 0.25 g/t gold. Intersections that are lower than this threshold may provide exploration insight and may therefore be disclosed.

About Lavras Gold

Lavras Gold Corp. (TSXV: LGC, OTCQX: LGCFF) is a Canadian exploration company focused on realizing the potential of a multi-million-ounce gold district in southern Brazil. Its Lavras do Sul Project is located in Rio Grande do Sul State and is primarily an intrusive hosted gold system of possible alkaline affinity. More than 24 gold prospects centred on historic gold workings have been identified on the property, which spans more than 22,000 hectares. Follow Lavras Gold on www.lavrasgold.com, as well as on LinkedIn, Twitter, and YouTube.

Contact information

Michael Durose, President & CEO, or Naomi Nemeth, Vice President, Investor Relations
+1-289-624-1377 | investor@lavrasgold.com

DISCLAIMER AND FORWARD-LOOKING INFORMATION

Neither the TSX Venture Exchange nor its Regulation Services Provider (as defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of the content of this news release.

This news release contains certain “forward-looking information” within the meaning of applicable securities laws. Forward-looking information is frequently characterized by words such as “plan”, “expect”, “project”, “intend”, “believe”, “anticipate”, “estimate”, “may”, “will”, “would”, “potential”, “proposed” and other similar words, or statements that certain events or conditions “may” or “will” occur. These statements, including those on planned exploration activities and goals, are only objectives and predictions. Forward-looking information is based on the opinions and estimates of management at the date the information is provided and is subject to a variety of risks and uncertainties and other factors that could cause actual events or results to differ materially from those projected in the forward-looking information, including the risks and factors that generally affect exploration and the uncertainty of exploration results. For a description of the risks and uncertainties facing the Company and its business, refer to the Company’s Management’s Discussion and Analysis recently filed under the Company’s profile on www.sedar.com. The Company undertakes no obligation to update forward-looking information if circumstances or management’s estimates or opinions should change, unless required by law. The reader is cautioned not to place undue reliance on forward-looking information.

FIGURE 1
Location of the Fazenda do Posto discovery relative to Butiá Gold Deposit, as well as the advanced gold discoveries at the LDS Project.

Location of the Fazenda do Posto discovery relative to Butiá Gold Deposit, as well as the advanced gold discoveries at the LDS Project.

FIGURE 2
Fazenda do Posto Drill holes -Plan View Showing location of Drill Holes 23FP001, 23FP002, 23FP003, 23FP004 and 23FP006.

Fazenda do Posto Drill holes -Plan View Showing location of Drill Holes 23FP001, 23FP002, 23FP003, 23FP004 and 23FP006.

FIGURE 3
Cross section of Fazenda do Posto Drilling looking west. Hole 23FP002 returned 340 metres grading 1.1 grams per tonne gold from 117 metres. Hole 23FP006 was collared 210 metres northeast of hole 23FP002 and returned 230 metres grading 0.9 grams per tonne gold from 31 metres and including 65 metres grading 1.9 grams per tonne gold. 23FP003 returned 108 metres grading 0.8 grams per tonne gold from 87 metres. Salmon colour represents the Fazenda do Posto granodiorite, yellow is episyenite, pink is perthitic granite. Note scale at bottom of hole. 1 ppm gold = 1 gram per tonne

Cross section of Fazenda do Posto Drilling looking west. Hole 23FP002 returned 340 metres grading 1.1 grams per tonne gold from 117 metres. Hole 23FP006 was collared 210 metres northeast of hole 23FP002 and returned 230 metres grading 0.9 grams per tonne gold from 31 metres and including 65 metres grading 1.9 grams per tonne gold.  23FP003 returned 108 metres grading 0.8 grams per tonne gold from 87 metres. Salmon colour represents the Fazenda do Posto granodiorite, yellow is episyenite, pink is perthitic granite. Note scale at bottom of hole. 1 ppm gold = 1 gram per tonne

FIGURE 4
Typical example of albitized and potassic altered mineralized episyenite from drill hole 23FP003. The rock consists of 95-96% brick red to whitish red potassium feldspar and albite, 1% black to dark green Fe-rich chlorite, 1-2% pyrite+- arsenian pyrite and 1% white to gray carbonate. This sample is from drill hole 23FP003 from 123 to 124 metres and grades 2.873 g/t gold.

Typical example of albitized and potassic altered mineralized episyenite from drill hole 23FP003. The rock consists of 95-96% brick red to whitish red potassium feldspar and albite, 1% black to dark green Fe-rich chlorite, 1-2% pyrite+- arsenian pyrite and 1% white to gray carbonate. This sample is from drill hole 23FP003 from 123 to 124 metres and grades 2.873 g/t gold.

FIGURE 5
Typical example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and albite, 2-3% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 1-3% disseminated pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 120 to 121 metres. This interval grades 1.405 g/t gold. The brick red colouration in the feldspar is from iron and barium. Note that the feldspar grain boundaries are sub-rounded to sub-angular reflecting pervasive metasomatic alteration likely from alkaline fluids.

Typical example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and albite, 2-3% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 1-3% disseminated pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 120 to 121 metres. This interval grades 1.405 g/t gold. The brick red colouration in the feldspar is from iron and barium. Note that the feldspar grain boundaries are sub-rounded to sub-angular reflecting pervasive metasomatic alteration likely from alkaline fluids.

FIGURE 6
High-grade example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and whitish pink albite, 1-2% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 3-4% disseminated to network textured pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 160 to 161 metres. This interval grades 8.053 g/t gold.

High-grade example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and whitish pink albite, 1-2% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 3-4% disseminated to network textured pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 160 to 161 metres. This interval grades 8.053 g/t gold.

TABLE 1
Summary table of metre-by-metre drilling assay results from drill hole 23FP006 on Fazenda do Posto target.

HoleAzimuth
(degrees)
Dip
(degrees)
End of hole
(metres)
From
(metres)
To
(metres)
Gold interval
(metres)
Gold grade
(g/t)
Lithology
23FP006200-60299.8331.132.00.90.31Episyenite
    33.035.02.00.14Episyenite
    35.037.02.00.11Episyenite
    37.039.02.00.35Episyenite
    39.041.02.00.02Episyenite
    41.043.02.00.01Episyenite
    43.045.02.00.01Episyenite
    45.047.02.00.02Episyenite
    47.048.01.00.32Episyenite
    48.049.01.00.55Episyenite
    49.050.41.40.01Episyenite
    50.451.71.30.01Episyenite
    51.753.01.30.01Episyenite
    53.054.01.00.01Episyenite
    54.055.01.00.34Episyenite
    55.056.01.00.74Episyenite
    56.057.01.00.41Episyenite
    57.058.01.00.50Episyenite
    58.059.01.00.62Episyenite
    59.060.01.00.65Episyenite
    60.061.01.00.50Episyenite
    61.062.01.00.35Episyenite
    62.063.01.00.30Episyenite
    63.064.01.00.43Episyenite
    64.065.01.00.24Episyenite
    65.066.01.00.57Episyenite
    66.067.01.00.42Episyenite
    67.068.01.00.16Episyenite
    68.069.01.00.47Episyenite
    69.070.01.00.41Episyenite
    70.071.01.00.26Episyenite
    71.072.01.00.40Episyenite
    72.073.01.00.45Episyenite
    73.074.01.00.27Episyenite
    74.075.01.00.52Episyenite
    75.076.01.00.44Episyenite
    76.077.01.00.92Episyenite
    77.078.01.00.70Perthitic granite
    78.079.01.00.42Episyenite
    79.080.01.00.34Episyenite
    80.081.01.00.50Episyenite
    81.082.01.00.68Episyenite
    82.083.01.01.04Episyenite
    83.084.01.00.59Episyenite
    84.085.01.00.87Episyenite
    85.086.01.00.92Episyenite
    86.087.01.01.62Episyenite
    87.088.01.01.21Episyenite
    88.089.01.00.71Episyenite
    89.090.01.00.45Episyenite
    90.091.01.00.89Episyenite
    91.092.01.00.59Episyenite
    92.093.01.01.37Episyenite
    93.094.01.01.81Episyenite
    94.095.01.01.33Episyenite
    95.096.01.00.50Episyenite
    96.097.01.01.72Episyenite
    97.098.01.00.95Episyenie
    98.099.01.01.12Episyenite
    99.0100.01.01.09Episyenite
    100.0101.01.00.94Episyenite
    101.0102.01.00.67Episyenite
    102.0103.01.00.92Episyenite
    103.0104.01.00.73Episyenite
    104.0105.01.00.83Episyenite
    105.0106.01.01.13Episyenite
    106.0107.01.00.82Episyenite
    107.0108.01.00.54Episyenite
    108.0109.01.00.49Episyenite
    109.0110.01.01.06Episyenite
    110.0111.01.00.73Episyenite
    111.0112.01.01.01Episyenite
    112.0113.01.00.91Episyenite
    113.0114.01.00.36Episyenite
    114.0115.01.00.29Episyenite
    115.0116.01.00.11Episyenite
    116.0117.01.00.17Episyenite
    117.0118.01.00.42Episyenite
    118.0119.01.00.70Episyenite
    119.0120.01.00.53Episyenite
    120.0121.01.01.41Episyenite
    121.0122.01.00.66Episyenite
    122.0123.01.00.50Episyenite
    123.0124.01.00.59Episyenite
    124.0125.01.01.38Episyenite
    125.0126.01.00.02Episyenite
    126.0127.01.00.89Episyenite
    127.0128.01.00.64Episyenite
    128.0129.01.00.71Episyenite
    129.0130.01.00.44Episyenite
    130.0131.01.00.53Episyenite
    131.0132.01.00.41Episyenite
    132.0133.01.00.16Perthitic Granite
    133.0134.01.00.01Perthitic Granite
    134.0135.01.00.14Perthitic Granite
    135.0136.01.00.90Episyenite
    136.0137.01.01.09Episyenite
    137.0138.01.01.03Episyenite
    138.0139.01.00.29Episyenite
    139.0140.01.00.51Episyenite
    140.0141.01.00.57Episyenite
    141.0142.01.00.52Episyenite
    142.0143.01.00.81Episyenite
    143.0144.01.00.47Episyenite
    144.0145.01.02.43Episyenite
    145.0146.01.00.16Episyenite
    146.0147.01.00.12Episyenite
    147.0148.01.00.10Episyenite
    148.0149.01.00.12Episyenite
    149.0150.01.02.04Episyenite
    150.0151.01.02.91Episyenite
    151.0152.01.02.22Episyenite
    152.0153.01.02.11Episyenite
    153.0154.01.00.83Episyenite
    154.0155.01.02.92Episyenite
    155.0156.01.02.04Episyenite
    156.0157.01.03.19Episyenite
    157.0158.01.03.94Episyenite
    158.0159.01.02.02Episyenite
    159.0160.01.00.67Episyenite
    160.0161.01.08.05Episyenite
    161.0162.01.01.90Episyenite
    162.0163.01.01.75Episyenite
    163.0164.01.03.13Episyenite
    164.0165.01.00.98Episyenite
    165.0166.01.01.28Episyenite
    166.0167.01.02.47Episyenite
    167.0168.01.02.66Episyenite
    168.0169.01.01.47Episyenite
    169.0170.01.02.13Episyenite
    170.0171.01.01.85Episyenite
    171.0172.01.01.33Episyenite
    172.0173.01.00.82Episyenite
    173.0174.01.01.13Episyenite
    174.0175.01.01.99Episyenite
    175.0176.01.00.79Episyenite
    176.0177.01.01.69Episyenite
    177.0178.01.01.97Episyenite
    178.0179.01.01.47Episyenite
    179.0180.01.01.29Episyenite
    180.0181.01.02.30Episyenite
    181.0182.01.01.04Episyenite
    182.0183.01.00.68Episyenite
    183.0184.01.02.08Episyenite
    184.0185.01.02.94Episyenite
    185.0186.01.00.73Episyenite
    186.0187.01.02.47Episyenite
    187.0188.01.00.96Episyenite
    188.0189.01.00.64Episyenite
    189.0190.01.01.44Episyenite
    190.0191.01.03.01Episyenite
    191.0192.01.02.26Episyenite
    192.0193.01.01.56Episyenite
    193.0194.01.01.33Episyenite
    194.0195.01.02.10Episyenite
    195.0196.01.01.39Episyenite
    196.0197.01.02.17Episyenite
    197.0198.01.01.74Episyenite
    198.0199.01.01.72Episyenite
    199.0200.01.01.65Episyenite
    200.0201.01.01.77Episyenite
    201.0202.01.02.51Episyenite
    202.0203.01.01.86Episyenite
    203.0204.01.01.54Episyenite
    204.0205.01.04.07Episyenite
    205.0206.01.01.22Episyenite
    206.0207.01.01.25Episyenite
    207.0208.01.01.20Episyenite
    208.0209.01.01.44Episyenite
    209.0210.01.01.34Episyenite
    210.0211.01.00.23Perthitic Granite
    211.0212.01.00.72Perthitic Granite
    212.0213.01.02.18Perthitic Granite
    213.0214.01.02.59Perthitic Granite
    214.0215.01.00.32Perthitic Granite
    215.0216.01.00.14Perthitic Granite
    216.0217.01.00.14Perthitic Granite
    217.0218.01.00.69Perthitic Granite
    218.0219.01.00.04Perthitic Granite
    219.0220.01.00.08Perthitic Granite
    220.0221.01.00.36Perthitic Granite
    221.0222.01.00.18Perthitic Granite
    222.0223.01.00.10Perthitic Granite
    223.0224.01.00.01Perthitic Granite
    224.0225.01.00.09Perthitic Granite
    225.0226.01.00.16Perthitic Granite
    226.0227.01.00.02Perthitic Granite
    227.0228.01.00.02Perthitic Granite
    228.0229.01.00.13Perthitic Granite
    229.0230.01.00.12Perthitic Granite
    230.0231.01.00.11Perthitic Granite
    231.0232.01.01.31Perthitic Granite
    232.0233.01.00.05Perthitic Granite
    233.0234.01.00.20Perthitic Granite
    234.0235.01.00.33Perthitic Granite
    235.0236.01.00.01Perthitic Granite
    236.0237.01.00.01Perthitic Granite
    237.0239.02.00.01Perthitic Granite
    239.0241.02.00.01Perthitic Granite
    241.0243.02.00.04Perthitic Granite
    243.0245.02.00.02Perthitic Granite
    245.0247.02.00.02Perthitic Granite
    247.0249.02.00.06Perthitic Granite
    249.0250.01.00.03Perthitic Granite
    250.0251.01.00.08Perthitic Granite
    251.0252.01.00.20Perthitic Granite
    252.0253.01.00.03Perthitic Granite
    253.0254.01.00.02Perthitic Granite
    254.0255.01.00.07Perthitic Granite
    255.0256.01.00.10Perthitic Granite
    256.0257.01.01.84Perthitic Granite
    257.0258.01.00.26Perthitic Granite
    258.0259.01.00.25Perthitic Granite
    259.0260.01.00.61Perthitic Granite
    260.0261.01.00.16Perthitic Granite
    261.0262.01.00.08Perthitic Granite
    262.0263.01.00.01Perthitic Granite
    263.0264.01.00.01Perthitic Granite
    264.0265.01.00.01Perthitic Granite
    265.0267.02.00.02Perthitic Granite
    267.0269.02.00.01Perthitic Granite
    269.0271.02.00.02Perthitic Granite
    271.0273.02.00.01Perthitic Granite
    273.0275.02.00.01Perthitic Granite
    275.0277.02.00.01Perthitic Granite
    277.0279.02.00.01Perthitic Granite
    279.0281.02.00.01Perthitic Granite
    281.0283.02.00.01Perthitic Granite
    283.0285.02.00.01Perthitic Granite
    285.0287.02.00.01Perthitic Granite
    287.0289.02.00.01Perthitic Granite
    289.0291.02.00.01Perthitic Granite
    291.0293.02.00.01Perthitic Granite
    293.0295.02.00.01Perthitic Granite
    295.0297.02.00.01Perthitic Granite
    297.0299.82.80.01Perthitic Granite

Notes

  • Assumes 0.25 g/t gold cut-off grade, no top cut.
  • The Company has been targeting larger intersections of greater than 0.25 g/t gold. Intersections that are lower than this threshold may provide exploration insight and may therefore be disclosed.
  • Intervals represent drill core interval; true widths have not been determined at this time.

TABLE 2
Summary of Drill hole Assay Results for Fazenda do Posto target.

HoleAzimuth

(degrees)
Dip

(dip)
End of hole

(metres)
From

(metres)
To

(metres)
Interval

(metres)
Gold grade

(grams/tonne)
Comment
23FP00120-60214.0577.00153.0076.000.17Drilled peripheral to main target
    85.0086.001.000.32Along southeast edge of FP
    90.0093.003.000.33 
    96.0097.001.000.57 
    102.00104.002.000.34 
    109.00110.001.000.42 
    113.00118.005.000.23 
    135.00137.002.000.47 
    143.00144.001.000.26 
23FP00220-60464.5958.0059.001.000.18Discovery hole
    117.00457.00340.001.09Mineralized episyenite
   Including199.00359.00160.001.79 
   Including208.00235.0027.002.07 
   Including293.00361.0068.002.09 
         
23FP0030-90332.1724.0027.003.000.71 
    87.00294.00207.000.49 
   including87.00227.00140.000.67 
   Including87.00195.00108.000.80 
   Including87.00151.0064.000.91Mineralized episyenite
   Including87.00145.0058.000.97 
   Including106.00145.0039.001.17 
         
HoleAzimuth

(degrees)
Dip

(degrees)
End of hole

(metres)
From

(metres)
To

(metres)
Interval

(metres)
Gold grade

(grams/tonne)
Comment
23FP004200-60 No Significant Value   Drilled southwest away from target
         
23FP006200-60 31.06261.00229.940.86Drilled southwest into target
   including31.06235.00203.940.95Mineralized episyenite
   including31.06222.00190.941.00 
   including149.00214.0065.001.94 
   including149.00187.0038.002.03 
   including154.00164.0010.002.96 
   including190.00205.0015.002.05 


Photos accompanying this announcement are available at

https://www.globenewswire.com/NewsRoom/AttachmentNg/ea7a7867-98b3-4e16-99d1-e4ebe70756cf

https://www.globenewswire.com/NewsRoom/AttachmentNg/97bb634b-f8bc-4c99-bbb2-657b22f3e6a4

https://www.globenewswire.com/NewsRoom/AttachmentNg/5fea2c5d-a5e9-4630-9ed3-706a4563bc73

https://www.globenewswire.com/NewsRoom/AttachmentNg/335d0848-3b4b-4158-866f-31ccfaab3a5b

https://www.globenewswire.com/NewsRoom/AttachmentNg/6be0bbc9-1629-4751-8f02-9cd6c181d2bc

https://www.globenewswire.com/NewsRoom/AttachmentNg/05e1bfa3-efb8-432c-be20-505ddb2fc047


Primary Logo

Figure 1

Location of the Fazenda do Posto discovery relative to Butiá Gold Deposit, as well as the advanced gold discoveries at the LDS Project.
Figure 2

Fazenda do Posto Drill holes -Plan View Showing location of Drill Holes 23FP001, 23FP002, 23FP003, 23FP004 and 23FP006.
Figure 3

Cross section of Fazenda do Posto Drilling looking west. Hole 23FP002 returned 340 metres grading 1.1 grams per tonne gold from 117 metres. Hole 23FP006 was collared 210 metres northeast of hole 23FP002 and returned 230 metres grading 0.9 grams per tonne gold from 31 metres and including 65 metres grading 1.9 grams per tonne gold. 23FP003 returned 108 metres grading 0.8 grams per tonne gold from 87 metres. Salmon colour represents the Fazenda do Posto granodiorite, yellow is episyenite, pink is perthitic granite. Note scale at bottom of hole. 1 ppm gold = 1 gram per tonne
Figure 4

Typical example of albitized and potassic altered mineralized episyenite from drill hole 23FP003. The rock consists of 95-96% brick red to whitish red potassium feldspar and albite, 1% black to dark green Fe-rich chlorite, 1-2% pyrite+- arsenian pyrite and 1% white to gray carbonate. This sample is from drill hole 23FP003 from 123 to 124 metres and grades 2.873 g/t gold.
Figure 5

Typical example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and albite, 2-3% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 1-3% disseminated pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 120 to 121 metres. This interval grades 1.405 g/t gold. The brick red colouration in the feldspar is from iron and barium. Note that the feldspar grain boundaries are sub-rounded to sub-angular reflecting pervasive metasomatic alteration likely from alkaline fluids.
Figure 6

High-grade example of gold mineralization in episyenite from drill hole 23FP006. The rock consists of 95% brick red potassium feldspar and whitish pink albite, 1-2% black to dark green iron-rich chlorite, 1-2% grey and white carbonate vesicles, and 3-4% disseminated to network textured pyrite and arsenian pyrite. This example is from drill hole 23FP006 from 160 to 161 metres. This interval grades 8.053 g/t gold.