Subscribers,

A few weeks ago we introduced you to BGADF, and it rewarded us with some 18% gains.

Today, the Company announced some big news so it is back in focus.

Brigadier Intercepts 12.62 g/t Gold and 78 g/t Silver with 4.5% Copper Across 0.8 Metres at Picachos

Underground Sampling from Undrilled Surrounding Veins Returns 109.14 g/t Gold and 20 g/t Silver Across 0.5 Metres

VANCOUVER, BC / ACCESSWIRE /February 17, 2021 / Brigadier Gold Limited (the "Company" or "Brigadier") (TSXV:BRG)(FSE:B7LM)(OTC PINK:BGADF) is pleased to provide additional diamond drill and underground sampling results from ongoing phase one exploration at its Picachos gold-silver project, Sinaloa Mexico (the "Picachos Project", "Picachos" or the "Property"). Brigadier has completed and received assay results for 3085 metres of diamond drilling in 28 holes on the Picachos Project. Assays results for holes 21 through 28 and recent underground sampling are provided in Table 1.

Phase-one exploration highlights to date:

• Confirmed seven-kilometre-long vein system of precious metals mineralization

• Widely spaced holes show vein continuity on strike and at depth with robust width

• High grade nature of precious metals mineralization consistently observed in assays

• Confirmed meaningful gold/silver mineralization in hanging wall and footwall of vein systems

• Discovered previously unexplored high-grade gold and silver historic workings

• Multiple new surface and subsurface targets discovered during reconnaissance and mapping

• Copper porphyry target sampling suggests high priority follow-up exploration

Geologist and Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects ("NI 43-101"), Michelle Robinson comments "results of our phase-one program at Picachos imply a robust and geographically expansive mineralized system for which we have only just scratched the surface. I am very pleased with our results, in particular the number of targets demanding follow up drilling or for newly discovered zones, a first ever drill hole. The Cocolmeca vein structure (CVS) is persistent and strongly mineralized and I look forward to expanding the depth and strike length in 2021, as well as continuing the exploration of the rest of the CVS, particularly in the central Cocolmeca area."

Of the 28 holes drilled to date, fourteen (1704 metres) were drilled to test the San Agustín Vein, 10 holes (1029 metres) tested surface exploration targets defined by trenching, 2 holes (168 metres) tested under the historic San Antoñio Mine and one hole tested under the historic La Gloria Mine. San Agustín and San Antoñio represent two gold-rich, polymetallic mineral chutes about 2.5 kilometres apart on Brigadier's regional-scale Cocolmeca Vein System (CVS), and La Gloria historically produced gold from a northwesterly trending vein roughly orthogonal to the CVS. The CVS has been defined at varying levels of certainty along the east-northeasterly trending diagonal of the Property for more than seven kilometres.

La Gloria Gold Mine and Palodismo
La Gloria underground gold mine is accessed from a 106 metre long east-southeasterly trending cross-cut located at 965 metres elevation in the central part of the Property. This opening provides access to a southeasterly trending stope that is more than 70 metres long and about 1.5 metres wide. Historic sample MTA-15659 was cut across the northwest face of this stope and contained values of 21.09 g/t Au, 6.6 g/t Ag, 0.4% Cu, 0.8% Pb and 0.5% Zn across 0.8 metres. The orientation of the structure at this location is 162°/75° SW. Brigadier cut a sample across the southeastern face of the stope which returned a result of 49.6 g/t Au and 31 g/t Ag across 0.4 metres (BRG-26402) and a notably more easterly orientation of 150°/74° SW. Mineralization in the stope consists of microcrystalline quartz breccia intergrown with pink epidote (piemontite?), and native gold along a shear zone hosted in agglomerate. The mud matrix between volcanic blocks and bombs is pervasively replaced by microcrystalline grey quartz intergrown with galena, sphalerite and lesser chalcopyrite.

Palodismo was first identified in historic sample MTA-19690 with results of 27.61 g/t Au and 4 g/t Ag across 1.3 metres from a small underground prospect 65 metres north of the entrance to La Gloria. Characteristic "pink epidote-quartz" is mentioned in the notes from 2007. A second underground prospect 115 metres SE of La Gloria cross-cut was sampled by Brigadier with results of 9.7 g/t Au and 2 g/t Ag across 0.8 metres (BRG-25207). Measured vein orientations from both prospects are 147°/75° SW.

Drill hole BRG-028 was collared 72 metres southwest of La Gloria. It was designed to intercept both Palodismo and La Gloria under historic sample MTA-15657 with a result of 5.27 g/t Au and 7 g/t Ag across 1.5 metres. All of DH-BRG-028 was altered to propylitic mineral assemblages dominated by epidote and chlorite. Microcrystalline galena and sphalerite in silicified mud between volcanic blocks and bombs defines a broad geochemical response of 0.4% Zn, 0.2% Pb, 170 ppm Cu, 0.2 g/t Au and 2 g/t Ag along the entire hole length of 183.5 metres. The section between 59 and 64 metres contains 1.2% Zn and 0.3% Pb with 348 ppm Cu across 5 metres. Shear zones marked by kaolinite and/or and pink quartz-piemontite breccias contain elevated gold values. Several of these were intercepted in the hanging wall to Palodismo. One of these contains 1.8 g/t Au and 1.9 g/t Ag across 2 metres between 35 and 37 metres. Palodismo itself is defined by a geochemical anomaly of 2.29 g/t Au across 8 metres between 105 and 113 metres. The Palodismo Vein is marked by pink quartz-epidote breccia between 110 and 111 metres with values of 10.65 g/t Au across 1 metre. A three-point solution between MTA-19690, BRG-25207 and this intercept in DH-BRG-028 yields an orientation of 145°/73° SW, in good agreement with field measurements from underground exposures of Palodismo.

A second intercept of 6.26 g/t Au between 141 and 142 metres in DH-BRG-028 is only tentatively correlated to La Gloria Vein. This interpretation implies that the vein flattens out at depth to a dip of about 65 degrees. Alternatively, the strike may have changed as implied by BRG-26402, and DH-BRG-028 never reached La Gloria Vein. Further drilling is required to clearly define La Gloria Vein at depth.

 

Figure 1. Geological cross-section of DH-BRG-028.

 

Figure 2. Level Plan 965 metre of La Gloria. Only the Adit and MTA-15659, MTA-15657 and BRG-26402 are in this plane. Everything else is above (BRG-25207) or below (MTA-19690, DH-BRG-028).

San Antoñio
San Antoñio is a historic prospect cut across the major ENE trending Cocolmeca Vein system that bisects the Property along the 8 km ENE diagonal 250 metres northwest of La Gloria Gold Mine. Values of 44.1 g/t Au, 47 g/t Ag, 0.4% Cu, 0.2% Pb and 0.7% Zn across 0.8 metres were obtained in historic sample MTA-19856. A prior operator drilled RC hole TAN3 under MTA-19856 in 2008 and got a result of 0.8% Cu, 0.29 g/t Au, 451 ppm Pb and 525 ppm Zn across 1.02 metres between 84.66 metres and 85.68 metres down-hole. Brigadier decided that historic result did not make sense considering the high-grade nature of this large, continuous vein. To clarify this view, two PQ diamond core holes were drilled with pierce points into La Coco on either side of TAN3. DH-BRG-026, cut northeast of TAN3, yielded a result of 1.07 g/t Au, 18 g/t Ag, 0.4% Cu, 0.2% Zn across 3.9 metres between 74 and 77.9 metres. This result includes 4.44 g/t Au, 6 g/t Ag, 0.1% Cu across 0.9 metres between 77 and 77.9 metres. DH-BRG-027, cut southwest of TAN3, intercepted a vein of semi-massive chalcopyrite with 12.62 g/t Au, 78 g/t Ag, 4.5% Cu, 0.2% Zn, 0.2% Pb across 0.8 metres between 54.7 and 55.5 metres down-hole. Both intercepts have significant hangingwall and footwall alteration comprised of piemontite, sphalerite, galena, pyrite and chalcopyrite (similar to La Gloria). From this data Brigadier concludes that the RC drilling method used previously was inadequate for sampling the Veins on this Property, although it was successful in locating the Veins in the subsurface.

 

Figure 3. Cross Section of DH-BRG-027

 

Figure 4. Geological Level Plan 740 metre of San Antoñio.

Nearby NW trending Veins
Several underground mines and prospects are developed on near-parallel veins within 500 metres to the southwest of La Gloria. These include Colorín, El Salvador, Urrea and Mangos. Of these, Urrea is the best developed with extraction levels at 840 metre, 860 metre, 895 metre, 935 metre and 1040 metre. Underground rock chip-channel results from these Veins include:

• 20.14 g/t Au and 36 g/t Ag across 1 metre in Sample BRG-25203 from Colorín Vein

• 11.55 g/t Au and 3 g/t Ag across 2 metre in Sample BRG-27376 from El Salvador Vein

• 109.14 g/t Au and 20 g/t Ag across 0.5 metre in Sample BRG-27405 from Urrea Vein (860 metre Level)

• 20.21 g/t Au and 22 g/t Ag with 19.4% lead across 0.3 metre in Sample BRG-25235 from Urrea Vein (1034 metre Level)

• 23.45 g/t Au and 6 g/t Ag in sample BRG-23762 from Mangos Vein

Ongoing Exploration
The Company has located and mapped several underground drifts and cross-cuts northwest of Lentes (Company PR dated 6 October) and near the Cobre Veins. A new batch of 224 underground and trench samples has been received by SGS laboratories. Results will be published when these are available from the Lab.

Appendix
Results from PQ diamond drill core holes and rock chip-channel sampling. DL=near detection limit, HW=hangingwall, FW=footwall.

	From (m)	To (m)	Core or Trench Width (m)	Estimated True Width (m)	Gold (g/t)	Silver (g/t)	Copper (ppm)	Lead (ppm)	Zinc (ppm)	Mo (ppm)	Area
Drill Hole
DH-BRG-021	10	11	1	unk	0.07	22	15	142	42	53
DH-BRG-022	21	22	1	unk	0.01	1	193	48	117	DL	Mochomos
DH-BRG-023	15	16	1	unk	DL	1	210	29	115	DL	Mochomos
DH-BRG-024	13.5	16.5	3	unk	0.01	1	355	21	125	DL	Mochomos
DH-BRG-025	9	39	30	unk	1.27	212	40	237	1	1	Doña Chayo
DH-BRG-026	68.5	74	5.5	5.0	DL	DL	294	269	1932	DL	San Antoñio HW
DH-BRG-026	74	77.9	3.9	3.5	1.07	18	3938	315	1549	3	San Antoñio Vein
including	77	77.9	0.9	0.8	4.44	6	796	155	337	6
DH-BRG-026	77.9	85	7.1	6.4	DL	DL	101	485	1556		San Antoñio FW
DH-BRG-027	42	54	12	10.8	DL	DL	169	466	2177	DL	San Antoñio HW
DH-BRG-027	54	56	2	1.6	5.08	35	19048	758	2216	16	San Antoñio Vein
including	54.7	55.5	0.8	0.7	12.62	78	45050	1597	2256	31
DH-BRG-027	56	61.5	5.5	5.0	DL	2	464	31	193	DL	San Antoñio FW
DH-BRG-028	0	183.5	183.5	183.5	0.21	2	170	1887	3697	DL	La Gloria Area
including	20	21	1	0.9	0.89	DL	30	787	1032	DL	Palodismo HW 3
including	35	37	2	1.8	1.92	2	26	1074	1334	DL	Palodismo HW 2
including	41	43	2	1.8	0.34	7	567	3628	6703	DL	Palodismo HW 1
including	59	64	5	4.5	0.03	2	348	3433	11449	DL
including	74	75	1	0.9	0.52	4	348	3716	8772	DL	Palodismo HW
including	94	95	1	0.9	0.71	DL	38	1697	1403	DL
including	105	113	8	7.2	2.29	DL	24	690	298	DL	Palodismo Vein
and	110	111	1	0.9	10.65	DL	25	765	266	DL
including	141	142	1	1.0	6.26	DL	47	5368	2857	DL	La Gloria Vein (?)
Trench
BRG-26402	4.5	4.9	0.4	0.4	49.60	31	506	3422	3682	DL	La Gloria
BRG-25207	2.2	3	0.8	0.8	9.70	2	930	5260	3180	DL	Palodismo (Tiro de Juan Flores)
BRG-27354	4	6.6	2.6	2.6	2.32	DL	159	872	1418	DL	Palodismo HW
BRG-25203	2	3	1	1	20.14	36	1420	7390	25100	6	Colorín
BRG-27376	0.5	2.5	2	2	11.55	3	1170	2330	4740	DL	Salvador
BRG-27377	1.5	2.5	1	1	1.61	7	3030	4670	14400	DL	Salvador
BRG-27378	1.75	2.5	0.75	0.75	0.88	141	97100	1980	3780	2	Salvador
BRG-27398	1.6	2.3	0.7	0.7	7.95	43	32600	2240	312	11	Urrea L. 860
BRG-27405	3	3.5	0.5	0.5	109.14	20	703	469	848	2	Urrea L. 860
BRG-27375	1	5.5	4.5	4.5	2.56	4	1953	6425	8570	DL	Urrea L. 1040
BRG-25235	2	2.3	0.3	0.3	20.21	22	1250	194000	2770	DL	Urrea L. 1034
BRG-23762	1.4	2.6	1.2	1.2	23.45	6	413	1893	1236	10	Mangos
BRG-117001	0	20	20	20	DL	DL	138	77	173	257	Porphyry-Line 2569200
BRG-117001	87	123	36	36	DL	DL	50	213	187	239	Porphyry-Line 2569200
BRG-117023	0	69	69	69	DL	DL	89	68	183	242	Porphyry-Line 2569200
including	54	66	12	12	DL	DL	169	121	160	593	Porphyry-Line 2569200
BRG-12155	0	75	75	75	DL	DL	58	78	221	440	Porphyry-Line 2569200
including	0	31	31	31	DL	DL	55	109	272	846	Porphyry-Line 2569200
including	25	31	6	6	DL	DL	35	185	302	2148	Porphyry-Line 2569200

The Picachos land package was methodically assembled by Michelle Robinson (MASc., P.Eng., Geologist and Qualified Person) over 10 years ago. Michelle is a respected industry veteran who has worked in Mexico for over 20-years with a number of major mining companies. She has authored over 20 technical reports and published several papers for the Society of Economic Geologists. Michelle and her team are executing on our 5,000-metre diamond drill program - the first ever on this project

The project's location, situated 25 kilometres equidistant from two recent bonanza grade discoveries of Vizsla Resources and GR Silver and along the same mineralized trend, positions Picachos as a truly exciting opportunity for Brigadier Gold and our shareholders.

The 3,954 hectare Picachos Property is centered over the historic "Viva Zapata" National Mineral Reserve, Sinaloa, Mexico. It overlaps two mineralized systems, a porphyry copper-molybdenum system hosted by a Paleocene granite-granodiorite intrusive complex, and a gold-silver vein complex comprised of both east-northeasterly trending veins (La Cocolmeca Vein System) and northwesterly trending veins (El Placer System). Sericitic alteration related to the porphyry system has been mapped over the northwestern two-thirds of the Property. Quartz-biotite veinlets with chalcopyrite and bornite occur in the central part of this broad zone of sericitic alteration and imply the presence of a significant porphyry system at depth. La Colcomeca Vein system has been mapped from San Agustín Underground Gold Mine in the southwestern part of the Property to El Pino seven kilometres to the northeast. In the central part of the Property, the best exposure of the northwesterly trending system occurs between La Gloria Underground Gold Mine and the Urrea Gold Mines, located 630 metres southwest of La Gloria. In this area, other northwesterly trending veins between these veins include Paldodismo, Colorin, Salvador, Trompetas and Mangos. On the eastern part of the Property, Tatemales and La Botica define a four kilometre long trend.

The growing inventory of priority drill targets underscore the untapped potential of this particular region of Sierra Madre Occidental epithermal belt.

Please visit our website to learn more about Brigadier Gold.

Visit https://finance.yahoo.com/news/brigadier-intercepts-12-62-g-140000947.html


We are keeping BGADF on our radar for the rest of the week as we believe there could be more short term upside, possibly to the $0.30 level, the recent high from back in September.



BGADF just issued a big press release yesterday morning that could get the attention of investors and traders alike...

Brigadier Intercepts 9.49 g/t Gold and 24 g/t Ag across 3 Metres at Picachos

Drilling and Surface Sampling Results Indicate Primary Vein System Contains Over 7 Kilometres of Robust Mineralization

Drill Assay Results from Other Previously Untested Prospective Zones Expected During January

VANCOUVER, BC / ACCESSWIRE / January 19, 2021 / Brigadier Gold Limited (the "Company" or "Brigadier") (TSXV:BRG)(FSE:B7LM)(OTC PINK:BGADF) is pleased to provide additional diamond drill and surface sampling results from ongoing phase one exploration at its Picachos gold-silver project, Sinaloa Mexico (the "Picachos Project" or the "Property"). Brigadier has completed 3085 metres of diamond drilling in 28 holes on the Picachos Project. Assays are now available for 20 holes (Table 1), and samples from the remaining holes are in-progress at SGS Laboratory in Durango.

Drilling highlights include:

• 9.49 g/t Au and 24 g/t Ag across 3 m (88 to 91 m) in DH-BRG-008

• 6.24 g/t Au and 79 g/t Ag across 3 m (122.5 to 125.5 m) in DH-BRG-009

• 7.03 g/t Au and 110 g/t Ag across 3.5 m (137.5 to 141 m) in DH-BRG-012

• 6.75 g/t Au and 44 g/t Ag across 2.5 m (108.5 to 111 m) in DH-BRG-014

Geologist and Qualified Person Michelle Robinson comments "I am really pleased with our results so far from San Agustín. The structure is persistent and strongly mineralized. Although our sampling with a diamond drill is not perfect due to the challenging sub-surface conditions, it definitely indicates a robust gold-bearing vein of substantial width and strike length of over seven kilometers. I look forward to expanding the depth and strike length in 2021, as well as continuing the exploration of the rest of the CVS (Colomeca Vein System), particularly in the central Cocolmeca area where a swarm of northwesterly trending veins intersects the east-north-easterly trending Cocolmeca Vein System."

Ranjeet Sundher, President and CEO, also comments "We are impressed with the speed in which Michelle and her team is de-risking the Picachos Project and increasingly demonstrating its regional scale potential. With just a small portion of the asset explored to date, I'm looking forward to keeping shareholders abreast as we aggressively move forward to further define the Colomeca Vein System while also commencing examination of the large copper-molybdenum porphyry target located on the northern part of the Property."

Of the 28 holes drilled to date, fourteen (1704.28 metres) were drilled to test the San Agustín Vein, 10 holes (1029 metres) tested surface exploration targets defined by trenching, 2 holes (168.5 metres) tested under the historic San Antoñio Mine and one hole tested under the historic La Gloria Mine. San Agustín and San Antoñio represent two gold-rich, polymetallic mineral chutes about 2.5 kilometres apart on Brigadier's regional-scale Cocolmeca Vein System (CVS), and La Gloria historically produced gold from a northwesterly trending vein roughly orthogonal to the CVS. The CVS has been defined at varying levels of certainty along the east-northeasterly trending diagonal of the Picachos Project for more than seven kilometres. Six surface rock chip-channel results that help define the location of the CVS include:

1. 4.89 g/t Au and 67 g/t Ag across 5 metres (trench BRG-104705) from San Agustín (PR dated 24 November 2020)

2. 1.85 g/t Au and 4 g/t Ag across 10 metres (trench BRG-120920) at Los Tejones prospect pits, centered 1 kilometre northeast of San Agustín

3. 347 g/t Ag, 0.1 g/t Au and 5.2% Cu across 1.0 metres (historic trench MTA-15953) at Guayabo, 2.4 kilometres northeast of San Agustín

4. 44.09 g/t Au and 47 g/t Ag across 0.8 metres (historic trench MTA-19856) at San Antoñio, 2.5 kilometres northeast of San Agustín

5. 5.25 g/t Au and 74 g/t Ag across 1.2 metres (trench BRG-27012) from the road to La Botica, 3.7 kilometres from San Agustín

6. 1.9 g/t Au and 98 g/t Ag across 1.6 metres (trench BRG-25220) from El Pino, 5.8 kilometres northeast of San Agustín (PR dated 14 September 2020)

Figure 1. Overview map of surface results 1 to 6 (above) on the surface trace of the CVS, highlighted in yellow. Locations of 2020 diamond drill sites are marked in black circles labeled DH. Holes 26 and 27 are below trench site 4 (MTA-19856). The Picachos Project boundary is in navy blue. The internal concession that is held by a subsidiary of Fresñillo PLC is marked in grey. The yellow CVS dips northwesterly, into the center of the Property.

During the Fall of 2020, the Company primarily explored the down-dip potential of the southwestern most segment of the CVS that was historically exploited by Minas de Picacho from San Agustín Adit Level 646 in the 1990's. Three fences of holes were drilled up to 130 metres north of this adit, and three fences were drilled up to 90 metres south of Level 646. Overall, a strike length of about 210 metres was tested. Most mineral intercepts were located between 650 and 550 metres elevation. The deepest test was in DH-BRG-007 at 530 m elevation or 200 metres below topography.

Geologically, the mineralization is located at the faulted and sheared contact between metamorphosed, thickly laminated, sulfide-rich argillite of deep marine origin and porphyritic intermediate continental volcanic rocks correlated to the Tarahumara Formation. Fault damage on this regional-scale geological terrane boundary is profound with shearing and quartz veining evident at several locations in the hanging wall to the San Agustín Vein. On Figure 3, a preliminary interpretation of what this veining might look like is shown in the rose color in the Picachos Project fault block. Some results from quartz veins and veinlets in the hanging wall to the San Agustín Vein are:

• 2.71 g/t Au and 24 g/t Ag across 2 m (54 to 56 m) in DH-BRG-003

• 0.6 g/t Au and 34 g/t Ag across 2 m (52 to 54 m) in DH-BRG-005

• 0.73 g/t Au and 27 g/t Ag across 4 m (51 to 55 m) in DH-BRG-014

Figure 2. Long section of the San Agustín Vein, looking west northwesterly, showing principal results from diamond drilling, underground and surface sampling completed by the Company in the fall of 2020. This section displays data from 12.5 meters in front of and behind the plane of the page.

Figure 3. Level Plan of the San Agustín Vein. All 14 diamond drill holes intercepted gold-rich polymetallic mineralization at the faulted contact between metamorphic argillite of submarine origin (blue) and altered continental volcanic rocks correlated to the Tarahumara Formation (greens). In the hanging wall (Picachos Project fault block), there are several quartz veins and veinlets hosted in the argillite. In rose, a possible interpretation for some of the hanging wall intercepts is shown.

At Los Tejones, encouraging results of 1.85 g/t Au were cut across 10 meters in a surface trench (BRG-120920). About 50 meters to the northeast, a second trench cut 1 meter of 428 g/t Ag (BRG-119913). Rock discovered by both trenches was deeply weathered and structures controlling the mineralization were mostly not obvious. Drill testing under these anomalies returned anomalous base metals but subdued precious metals (DH-BRG-015 to 20). Geologically, disseminated and stockwork mineralization occurs at the faulted contact between magnetic andesitic volcanics that might be Jurassic in age, and intermediate volcanic rocks correlated to the Tarahumara Formation.

Results from other surface trenches include:

• 2.09 g/t Au and 170 g/t Ag across 1.2 m from the Casimiro Vein (BRG-27024)

• 8.84 g/t Au, 36 g/t Ag and 1.6% Pb across 2 m from El Roque Vein (BRG-120828)

• 5.25 g/t Au, 74 g/t Ag and 1.7% Cu across 1.2 m from La Cocolmeca Vein (BRG-27012)

Table 1. List of results from drill holes and trenches completed by the Company in the fall of 2020.

	From (m)	To (m)	Core or Trench Width (m)	Estimated True Width (m)	Gold (g/t)	Silver (g/t)	Copper (ppm)	Lead (ppm)	Zinc (ppm)	Area
Drill Hole
DH-BRG-001	43	44	1	unk	0.61	25	166	387	598
DH-BRG-001	75	82	7	5.2	7.45	51	321	1896	3373	San Agustín
including	75.5	78	2.5	1.9	20.58	68	648	4682	7853
including	76	77	1	0.8	45.63	82	1436	9866	16800
DH-BRG-002	46	47	1	unk	1.33	22	112	212	572
DH-BRG-002	93	97.5	4.5	3.4	2.89	50	288	1350	1274	San Agustín
including	93	95	2	1.5	6.12	52	363	1977	1133
DH-BRG-003	54	56	2	unk	2.71	24	162	589	875
DH-BRG-003	66	68	2	unk	0.16	27	158	469	1176
DH-BRG-003	78.5	79	0.5	unk	0.19	20	290	753	495
DH-BRG-003	123	125.5	2.5	1.5	0.24	24	181	858	741	San Agustín
DH-BRG-004	40	41	1	unk	0.80	24	126	440	1753
DH-BRG-004	63	74.5	11.5	9	1.04	44	182	720	1576	San Agustín
including	63.5	64.5	1	0.8	9.63	89	405	1567	3770
DH-BRG-005	52	54	2	unk	0.60	34	269	605	2492
DH-BRG-005	65	66	1	unk	4.87	17	145	364	572
DH-BRG-005	102.5	107.5	5	4	1.95	52	374	1543	2109	San Agustín
including	103.5	104.5	1	0.8	7.67	69	1141	4474	5718
DH-BRG-006	93	94	1	unk	0.75	56	188	268	293
DH-BRG-006	102.5	112	9.5	7.3	0.48	19	315	835	1891	San Agustín
including	102.5	103	0.5	0.4	4.87	11	534	3415	2755
DH-BRG-007	137.5	140.5	3	1.6	1.40	20	532	1755	2987	San Agustín
including	138	138.5	0.5	0.3	7.58	22	184	837	1059
DH-BRG-008	84	99	15	11	2.94	16	246	809	1650	San Agustín
including	88	91	3	2.2	9.49	24	535	1684	3199
DH-BRG-009	122.5	137	14.5	5	1.55	18	1306	2260	2531	San Agustín
including	122.5	125.5	3	1.1	6.24	79	5863	9534	9428
DH-BRG-010	81.5	86	4.5	3.3	1.20	14	340	1124	1825	San Agustín
including	82	84.5	2.5	1.9	1.99	17	433	1295	2732
DH-BRG-011	120.5	133.5	13	7	0.59	15	298	1096	1895	San Agustín
including	121	122	1	0.6	1.83	33	777	2732	5903
including	128.5	130	1.5	0.9	2.22	17	583	1805	3279
DH-BRG-012	137.5	146	8.5	6	3.05	52	1464	10071	18529	San Agustín
including	137.5	141	3.5	3.1	7.03	110	3263	22352	42177
DH-BRG-013	26	27	1	unk	0.71	22	103	146	581
DH-BRG-013	53	60	7	4.9	1.93	36	140	424	973	San Agustín
including	57	60	3	2.1	6.07	85	352	1140	2618
DH-BRG-014	51	55	4	unk	0.73	27	82	341	1398
DH-BRG-014	77.5	78	0.5	unk	1.34	5	102	44	104
DH-BRG-014	85	85.5	0.5	unk	0.44	22	129	360	1031
DH-BRG-014	108.5	128	19.5	11.5	1.35	26	203	577	1226	San Agustín
including	108.5	111	2.5	2.1	6.75	44	265	1184	2923
DH-BRG-015	79	80.5	1.5	unk	0.09	12	1217	6221	5359	Los Tejones
DH-BRG-016	121	122	1	unk	0.01	5	299	2593	3977	Los Tejones
DH-BRG-017	110	120	10	unk	0.33	1	48	386	849	Los Tejones
DH-BRG-018	88	89	1	unk	0.42	1	61	1026	1077	Los Tejones
DH-BRG-019	39	45	6	unk	0.34	1	29	24	61	Los Tejones
DH-BRG-020	55	73	18	unk	0.01	1	40	853	1266	Los Tejones
Trench
BRG-93958	3	10	7	7	0.39	53	167	608	963	San Agustín Surface
BRG-120604	0	1.5	1.5	1.5	7.53	113	306	1262	3005	San Agustín (Mojonera 20 m depth)
including	0.7	0.9	0.2	0.2	39.37	125	744	3561	7509
BRG-120601	0	1.55	1.55	1.55	15.49	109	546	2016	4906	San Agustín (Mojonera 23 m depth)
including	0.5	0.85	0.35	0.35	66.36	99	1670	6744	11000
BRG-27010	0	0.6	0.6	0.6	45.85	187	1608	11822	12465	San Agustín (Mojonera 20 m depth)
including	0	0.1	0.1	0.1	2.82	536	5412	47700	32800
including	0.1	0.6	0.5	0.5	54.46	117	847	4646	8398
BRG-120613	0	2	2	2	4.11	39	284	1655	2733	San Agustín Carrito
including	0	1	1	1	8.02	63	446	3025	4680
BRG-93976	31	32	1	1	3.21	184	134	1626	23800	San Agustín Surface
BRG-104705	0	5	5	5	4.89	67	1265	3926	6125	San Agustín Surface (Don Genardo Trench)
including	1	2	1	1	9.85	44	834	2392	5594
BRG-119913	18	39	21	unk	0.09	36	323	401	877	Los Tejones
including	19	20	1	unk	0.12	428	116	843	895
BRG-120920	31	65	34	unk	0.65	3	280	291	711	Los Tejones
including	37	47	10	unk	1.85	4	316	211	525
including	43	44	1	unk	6.45	6	185	105	397
BRG-120910	5	9	4	unk	0.90	10	927	569	1678	Los Tejones
BRG-120755	0	4.4	4.4	4.4	0.20	23	2534	5829	567	Los Tejones
BRG-119749	11	32	21	unk	0.02	1	101	183	516	Los Tejones
BRG-119836	0	21	21	unk	0.08	4	788	1854	305	Los Tejones
including	0	6	6	unk	0.24	9	2011	6003	344
BRG-122536	0	16	16	unk	1.10	6	227	2346	683	Roque
including	6	8	2	unk	8.84	36	897	16000	1479
BRG-122536	319	341	22	unk	DL	1	83	486	947
BRG-120796	0	6	6	3	0.47	33	1096	3651	1448	Casimiro
including	3	4	1	0.5	2.17	137	3751	17600	2031
BRG-27024	0	1.2	1.2	1.2	2.09	170	6668	14300	3375	Casimiro
BRG-120841	0	12	12	unk	0.32	48	5294	190	259	Mochomos
including	9	11	2	unk	1.47	166	15000	434	427
BRG-120828	0	4	4	4	1.20	4	780	2408	2006	Roque?
including	0	1	1	1	3.50	10	371	5806	506
BRG-27012	1	2.2	1.2	1.2	5.25	74	17000	458	5983	La Cocolmeca
BRG-122694	192	274	82	unk	DL	8	183	210	148
including	250	252	2	1.8	0.25	265	1978	7105	692	Casimiro
BRG-122871	0	133	133	unk	0.10	1	82	364	383
including	6	8	2	unk	1.34	1	87.4	151	239
including	36	38	2	unk	1.24	2	141	1858	359	Roque?
including	72	86	14	unk	0.28	1	114	912	846

The Picachos Project land package was methodically assembled by Michelle Robinson (MASc., P.Eng., Geologist, 43-101 QP) over 10 years ago. Michelle is a respected industry veteran who has worked in Mexico for over 20-years with a number of major mining companies. She has authored over 20 technical reports and published several papers for the Society of Economic Geologists. Michelle and her team are executing on our 5,000-metre diamond drill program - the first ever on this project

The Picachos Project's location, situated 25 kilometres equidistant from two recent bonanza grade discoveries of Vizsla Resources and GR Silver and along the same mineralized trend, positions Picachos Project as a truly exciting opportunity for Brigadier and our shareholders.

The 3,954 hectare Picachos Project is centered over the historic "Viva Zapata" National Mineral Reserve, Sinaloa, Mexico. It overlaps two mineralized systems, a porphyry copper-molybdenum system hosted by a Paleocene granite-granodiorite intrusive complex, and a gold-silver vein complex comprised of both east-northeasterly trending veins (La Cocolmeca Vein System) and northwesterly trending veins (El Placer System). Sericitic alteration related to the porphyry system has been mapped over the northwestern two-thirds of the Property. Quartz-biotite veinlets with chalcopyrite and bornite occur in the central part of this broad zone of sericitic alteration and imply the presence of a significant porphyry system at depth. La Colcomeca Vein system has been mapped from San Agustín Underground Gold Mine in the southwestern part of the Property to El Pino seven kilometres to the northeast. In the central part of the Property, the best exposure of the northwesterly trending system occurs between La Gloria Underground Gold Mine and the Urrea Gold Mines, located 630 metres southwest of La Gloria. In this area, other northwesterly trending veins between these veins include Paldodismo, Colorin, Salvador, Trompetas and Mangos. On the eastern part of the Property, Tatemales and La Botica define a four kilometre long trend.

The growing inventory of priority drill targets underscore the untapped potential of this particular region of Sierra Madre Occidental epithermal belt.

Please visit our website to learn more about Brigadier Gold.

National Instrument 43-101 Disclosure
The technical information in this press release has been reviewed by Michelle Robinson, MASc., P.Eng., a Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects ("NI 43-101"). Core and sample handling procedures are documented in the Company's press release dated October 21, 2020. Standard pulps, field duplicates, pulp duplicates and blanks are inserted into the sample stream. The samples were analyzed by SGS Laboratories in Durango using fire-assay methods for gold, and ICP methods with a 4-acid digestion for silver and base metals. SGS is an accredited laboratory. It is the QP's opinion that the technical information disclosed in this press release is reliable.

Source: https://finance.yahoo.com/news/brigadier-intercepts-9-49-g-140000701.html
 

About BGADF

Brigadier Gold Limited was formed to leverage what we believe will be the next major bull market in the natural resource sector, particularly precious metals. Our mandate is to acquire undervalued and overlooked projects with demonstrable potential for advancement. 

Led by a management team with decades of experience in mineral exploration and capital markets development, we are focused on advanced exploration opportunities in politically stable jurisdictions.

Picachos Project

Brigadier’s 100% controlled Picachos project is a 3,954 hectare gold and silver prospect located in Sinaloa State, Mexico

Prior to 2002, the mineral tenure was fractured by several small concessions until they were assembled into a contiguous land package between 2003 and 2012.

Picachos hosts over 160 underground historic mines, workings and prospects which have yet to undergo modern, systematic exploration and drilling.

Primary targets include under-explored gold veins within the historic San Augstin mine and La Gloria, a historic mine with rock samples containing 21.1 g/t Au and 6 g/t Ag across 0.8m (Sample #15659)

Overview

The 3954.1 Ha Picachos Property overlaps a significant porphyry system centered in Southern Sinaloa State, Mexico, near geographic co‐ordinates 105º45’W and 23º12’ N. Mining concessions that define the Property were acquired by staking between 2003 and 2012 over the former “Viva Zapata” Mineral Reserve, a project that was staked and explored by the Servicio Geologico Mexicano in the 1980’s (Bon‐Aguilar, 1987 and Rodriguez‐Rodriguez et al., 1984). 
 
Geographically, the Property overlaps part of the western foothills of the Sierra Madre Occidental, one of the world’s largest silicic igneous provinces (Aranda‐Gomez et al.,2003). Regional geochemical work by the SGM at the turn of the millennium highlighted the Reserve as one of the largest contiguous anomalies for gold and base metals in southern Sinaloa and Northern Nayarit.

Detailed Gold Geochemistry in Stream Sediments

Picachos is situated on one of the largest high-amplitude contiguous anomalies for gold and base metals in the western Sierra Madre with values up to 6841 ppb Au in fine-fraction, active channel stream sediments
Anomalous drainages are on the northeasterly trending Cocolmeca Fault (San Agustin historic mine) and northwesterly trending veins related to Oligocene and Miocene extension (El Placer, Mirador).
 

Killala Lake Project

Brigadier Gold Ltd. has entered into an option agreement with Rudolf Wahl and Mike Dorval, together doing business as the Wahl Group, to acquire a 100-per-cent interest in the Killala Lake South diamond property, consisting of 46 cell claim units located in Killala Lake, Foxtrap Lake area townships, Thunder Bay mining district, Ont., subject to reservation of royalties in favour of the Wahl Group.

Killala Lake Area Madonna Diamond Dyke

A 1 tonne sample was taken and processed at Kennecott DMS plant in 2007-2008. Over sixty macro diamonds, including eight commercial sized diamonds were recovered. Colours included white, green, yellow, brown and grey diamonds with an average grade of 0.23 carats for the first sample taken. About half of the one tonne sample was taken from the fine-grained, chilled margin portion of the dyke from which one would expect a low diamond carrying potential.
 
 The dyke is approximately 1 to 2 meters wide at outcrop with strike/dip-direction at 009/065. The rock is macro-cryptic and dark comprised of approximately 20% olivine (up to 0.5cm), up to 2% garnet with reaction rims (0.2 cm), and minor cox in dark grey crystalline matrix. Magnetic susceptibility values ranged up to 10 SL. Some highly weather/baked country rock xenoliths were present. The dyke is layered or branded and contains both macro-crystic portions and non-macro-crystic bands, which are generally closer to the contact. The Majority is macro-cryptic. The dyke can be traced in outcrop for approximately 50 meters.
 
The dyke intrudes into granitoids with <0.5 SI magnetic susceptibility, and dips 65 degrees at the hanging wall and 78 degrees at the footwall, so the diamond bearing dyke will have a larger width at depth.
 
 A ground magnetic survey and MMI survey was created within the surrounding area of the diamond dyke. These survey’s outlined a large kimberlite pipe target just to the south of the diamond dyke and other kimberlite targets within close vicinity of the diamond bearing dyke.


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