guadalupe y calvo gold-silver project chihuahua state, mexico · 2020. 8. 4. · • in july, 2018,...
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![Page 1: Guadalupe Y Calvo Gold-Silver Project Chihuahua State, Mexico · 2020. 8. 4. · • In July, 2018, Endeavour reduced the San Luis and San Luis NW claims (with 18,391.5 and 36,025.3177](https://reader036.vdocuments.net/reader036/viewer/2022071509/612da1ab1ecc515869424f50/html5/thumbnails/1.jpg)
www.edrsilver.com TSX: EDR | NYSE: EXK
July, 2020
Guadalupe Y Calvo Gold-Silver Project Chihuahua State, Mexico
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GUADALUPE Y CALVO OVERVIEW
• Well located property, excellent road access, good local infrastructure
• Historic gold-silver mining district, multiple vein structures <3 km long
• Low sulfidation epithermal veins, high grade “bonanza” orebodies
• Prolific production history, 2 million oz gold, 28 million oz silver
• Encouraging historic drill results < 4.12 gpt gold, 281 gpt silver over 2.5 m
• Historic Indicated Resource of 142,500 oz gold, 7.1 million oz silver
• 1.86 million tonnes @ 2.4 gpt gold, 120 gpt silver
• Resource wide open beneath post-mineral tuffs
• Exploration targets untested and open along strike, at depth
• Endeavour is seeking a partner or buyer for the project
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GUADALUPE Y CALVO PROPERTY LOCATION AND ACCESS
• Located in the town of Guadalupe y
Calvo, southwestern Chihuahua State,
México, approximately 300 km south of
Chihuahua City.
• The Project is accessible by highway
from Chihuahua City through the city of
Hidalgo de Parral, a major mining
center about a 3 hour drive from GyC
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GUADALUPE Y CALVO CONCESSIONS
Concession NameTitle
NumberTerm of Mineral
ConcessionHectares
Guadalupe 159362 29/10/73 to 28/10/23 100.0000
Ampl. de Guadalupe 211461 31/05/00 to 30/05/50 28.0000
Guadalupe Tres 224250 22/04/05 to 21/04/55 148.7341
Guadalupe Tres 224430 10/05/05 to 09/05/55 159.8364
La Bufa 219036 31/01/03 to 30/01/53 1,040.7594
La Bufa 1 222724 27/08/04 to 26/08/54 485.0000
La Bufa 2 223165 28/10/04 to 27/10/54 765.5000
El Chapito 164161 05/03/79 to 04/03/29 20.0000
Guadalupe Tres Fraccion Dos 240131 13/04/12 to 12/04/62 0.4049
Guadalupe Tres Fraccion Dos 240132 13/04/12 to 12/04/62 2.2650
Total 2,750.4998
• In July, 2012, Endeavour Silver completed the acquisition of the Guadalupe y Calvo
Project from AuRico Gold Inc., which consisted of eight mineral concessions covering
54,856.1 hectares.
• In 2014, Endeavour Silver acquired four concessions controlled by Minera Lincoln de
Mexico, S.A. de C.V. (Lincoln), with 2,311.2594 hectares. These concessions cover the
extensions of the Rosario vein, both to the northwest and to the southwest.
• In July, 2018, Endeavour reduced the San Luis and San Luis NW claims (with 18,391.5
and 36,025.3177 hectares respectively) which were part of the original acquisition
• Currently, the Guadalupe y Calvo Project consists of ten mineral concessions covering
2,750.4998 hectares, including several old adits and shafts. Endeavour Silver and its
subsidiaries control 100% of the mineral properties comprising the Project and there are
no underlying royalty agreements on the mineral properties.
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GUADALUPE Y CALVO EARLY HISTORY
1554 Spanish exploration of northern Mexico begins.
1567 First significant mineral discovery in Chihuahua State.
1600-1700 Other major mineral discoveries in Mexico include: Parral, Batopilas, Santa Eulalia, Marguarichi, Dolores and Naica districts.
1820 Mexico gains independence from Spain and Mexican government encourages foreign investment to develop the economy – a revival of mining begins
1835 Bonanza gold was discovered on the site of the Rosario vein outcrop and in a short time the town of Zorrilla was founded Guadalupe y Calvo).
1835-1838 Ochoa family begin consolidating district and by 1928 have sole ownership of the northern Zorrilla and Pertenencia portions of the Rosario breccia/vein
complex. The southern San Francisco portion of Rosario remains in the hands of local small miners for many years.
1838-1949 Ochoa family lease their holdings to two English mining companies. During this time bonanza graded ores were produced from both open pit and
underground workings. Operations were restricted by lease agreements to approximately 100 meters below surface and above.
1844 Output from these mining operations was large enough that the Mexican government erected a mint to coin the mines output.
1849 Properties reverted back to the Ochoa family, as mutually agreed terms for new leasehold agreements on the properties could not be reached.
1849-1865 District was worked primarily by small miners and gambosinos under agreements with the Ochoas.
1865 Henry Holderness, an American of British decent, purchases one half interest in the Ochoa properties. Holderness utilized the exploration shafts and
tunnels constructed by the English companies to develop and mine the Pertenencia and Zorrilla portions of the Rosario breccias/vein complex down to
approximately 200 meters below the surface. At this depth, dewatering the mine became too much of a problem so mining halted there
1871 Holderness deeded his interests back to the Ochoa family.
1871-879 Ochoas leased ground to gambosinos and mining and production continued in a haphazard fashion.
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GUADALUPE Y CALVO LATER HISTORY
1879-1888 Ochoas leased properties to various U.S. politicians and mining promoters; however, all these ventures failed due to the demands of the Ochoas family.
1888 Ochoa family lost claims by failure to perform minimal work requirements.
1889-1894 American mining group consolidated district and mining activities were limited to repossessing dump materials, a highly profitable venture.
1895 Tiburcio Garcia, a local merchant acquired all interests in district and sold them to Rosario Mining Company of Ft. Worth, Texas.
1895-1910 Rosario Mining operated the property and undertook extensive underground sampling programs until the property was sold to West Mexican Mines Ltd.
1910-1939 West Mexican operated a 50-ton per day mill with a cyanide recovery circuit and reported recoveries of 90 percent. In 1930s operations shifted from the
main Rosario breccias/vein complex to the east west striking Nankin structure. Known for almost 100 years, this was the first time any diligent
exploration and development has been taken on the structure.
1940 West Mexican continued production until they left the district in 1940.
1940-1978 Small miners and gambisinos operated mines at Guadalupe y Calvo.
1978 Compañia Minera Los Maples S.A. de C.V. acquired claims encompassing both the Rosario and Nankin structure, rehabilitated the old mill building and
installed a treatment plant with a flotation circuit, and used the recovery process Merrill Crowe circuit on a small heap leach. Production by Los Maples
was derived from a small open cut at the top of the Rosario outcrop and underground workings in the Nankin. Grades in the open cut were reported to
be 4.3 g/t gold and 312 g/t silver.
1980s CRM performed studies as part of the Mexican government’s program to stimulate mining. No exploration work was
performed. Contrastista Tormex S.A., a subsidiary of Lacana reviewed data with no actual exploration work performed.
1996 V-Fund Investments Ltd. acquired an option from Los Maples and performed limited mapping, sampling and bottle roll leach tests on surface samples.
1997 Minera Glamis S.A. de C.V., subsidiary of Glamis Gold Ltd., performed limited work of mapping and a surface and underground sampling program
1998-2000 Augusta Resource Corp. of Vancouver, BC, entered into an agreement with V-Fund and completed a small 9-hole RC drill program in 2000.
2006 Gammon Gold acquires Guadalupe y Calvo project in the context of an acquisition of Mexgold.
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GUADALUPE Y CALVO ENDEAVOUR EXPLORATION
• Exploration activities commenced in 2013 and concluded in 2018, focused on regional
exploration to add resources to those already detected in El Rosario mine.
• In 2016, an interpretation of ASTER-type satellite images was performed.
• At the end of 2016, an Aerial Flight of Geophysics was carried out over 3,000 linear kilometers
(including Magnetometry, Gamma Ray Spectrometry and VLF).
• Both surveys generated anomalies that were partially followed up by geological prospecting
• Approximately 4,600 geochemical samples were collected with respect to the properties.
• From these activities are highlighted the following prospective areas: San Carlos, Las
Truchas, Canoas, Nabogame, Milpillas, Mesa de la Reforma, Gallinas and El Chapito.
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GUADALUPE Y CALVO ASTER ANOMALIES
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GUADALUPE Y CALVO AEROMAGNETIC ANOMALIES
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GUADALUPE Y CALVO REGIONAL GEOLOGY
• The mining district of Guadalupe y Calvo is located within the
Sierra Madre Occidental metallogenic province, a north-
northwesterly trending linear volcanic belt (Figure 7.1). This
volcanic field, 1,500 km long and 200 km wide, is one of the
world’s largest epithermal precious metal terranes, hosting a
majority of Mexico’s gold and silver deposits. It extends from
south of Oaxaca and Chiapas to Arizona and New Mexico.
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GUADALUPE Y CALVO REGIONAL MINING DISTRICTS
• GyC lies in the heart of the Sierra Madre
Occidental gold-silver belt of low sulfidation,
epithermal mining districts
• Fresnillo’s San Julian mine lies 50 km to the
SE and Couer’s Palmerejo mine lies 150 km
to the NW
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GUADALUPE Y CALVO PROPERTY GEOLOGY
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GUADALUPE Y CALVO CORE TARGETS
Rosario
San Carlos
El Chapito
GYC
Exploration Targets
SAN CARLOS
▸ San Carlos
▸ Silvia
SAN CARLOS II
▸ El Martillo
▸ La Paz
▸ El Jabalí
▸ Las Arañas
▸ Los Venados
▸ La Escondida
ROSARIO
▸ Rosario-Nankin
EL CHAPITO
▸ El Chapito
▸ Santo Niño
▸ El Tejaban
▸ El Encino
▸ El Capulin
▸ La Manzanilla
▸ El Libramiento
▸ El Arroyo
▸ El Pinabete
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GUADALUPE Y CALVO MINERALIZATION
• The property covers the historic Rosario mine, with past production of 2 million ounces of
gold and 28 million ounces of silver. Historic operations were hindered by water
problems when the mine reached the valley floor which is why mining was not
pursued down dip.
• Guadalupe y Calvo is a classic gold-silver low sulfidation epithermal deposit with quartz-
adularia-sericite veins. The system contains veins, breccias and stockworks
hosting economically significant gold and silver sulfide mineralization with open-
space textures associated with volcanic related hydrothermal systems.
• The mine’s main structural feature is the northwest striking Rosario fault complex with a
total width of the mineralized zone up to 80 m. Historic underground mining widths
of high-grade gold-silver mineralization were up to 10 m.
• The second major vein is the east-west striking Nankin vein, which dips shallowly south
at 30°. This structure has an obvious deflection where it intersects the Rosario
vein, creating a complex pattern of stockwork and sheeted veinlets that provides a
possibility for bulk-mining either in open pit or large underground stopes.
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GUADALUPE Y CALVO ROCK SAMPLING
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GUADALUPE Y CALVO ROSARIO TREND
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GUADALUPE Y CALVO ROSARIO MINE GEOLOGY
• The wide hydrothermal
breccia of the Rosario Vein
system is covered by the
unconformable post-
mineral volcanics to the
southeast, and is down-
thrown by the Bufa Fault on
the order of 400 m vertically
to the northwest.
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GUADALUPE Y CALVOROSARIO VEINS
Schematic surface vein map of the Project, showing the main Veins.
Section 64-1 SW-NE (looking NW) - Typical transverse section showing the two major veins. The
section is drawn perpendicular to the Rosario Vein, but skew to the strike of the Nankin Vein which
is an E-W vein dipping approximately 30° south, that has suffered drag folding in the hanging wall of
the Rosario structure.
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GUADALUPE Y CALVO ROSARIO AREA
Photograph of cliffs formed by ignimbrites
of UVS with Exploration Camp shown in
valley bottom.
Typical outcrop of the Rosario Vein looking
NNW along strike, here showing an 11m
wide zone of strong veining and
hydrothermal breccias.
Outcrop of the Rosario VeinOpen stopes at the surface of the
Rosario vein, looking SE towards town.
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GUADALUPE Y CALVO ROSARIO RESOURCE (Aurico Long
Section)
Longitudinal section of the Rosario Vein,
looking Northeast, showing the Silver /
Gold Ratio of mineralized intercepts in the
Rosario Vein drilled by Aurico. Although
there is no district-wide trend, there
appears to be “feeders” associated with
higher Ag / Au ratios. Ore deposits in the
Sierra Madre tend to have Ag – base metal
roots, and this could be evidence of such a
root to the system here.
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GUADALUPE Y CALVO ROSARIO RESOURCES (Aurico)
Longitudinal Section of Rosario Vein,
showing indicated resources blocks
Longitudinal Section of Rosario Vein, showing
inferred resources blocks
Longitudinal Section of Nankin Vein, showing
indicated resources blocks
Longitudinal Section of Nankin Vein, showing
inferred resources blocks
Classification Ton Ag Au Ag Oz Au Oz
Indicated Resources
1,861,000 119.5 2.4 7,147,300 142,500
Classification Ton Ag Au Ag Oz Au Oz
Inferred Resources
154,000 93.8 2.1 464,600 10,600
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GUADALUPE Y CALVO SAN CARLOS AREA
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GUADALUPE Y CALVO SAN CARLOS TARGETS
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GUADALUPE Y CALVO EL CHAPITO AREA
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GUADALUPE Y CALVO EL CHAPITO TARGETS
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GUADALUPE Y CALVOEL CHAPITO AREA
(Lincoln Drilling Program)
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GUADALUPE Y CALVOEL CHAPITO AREA
(Lincoln Significant Drill Intercepts)
hole id dip
from to intercept core rec Au Ag Cu Pb Zn
(m) (m) (m) dia % gpt gptppm or
%
ppm or
%
ppm or
%
LB-DDH-001 -45 89.20 90.00 0.80 NTW 100 0.166 11.3 172 236 502
91.50 93.00 1.50 NTW 100 0.178 11.4 145 222 304
94.50 97.00 2.50 NTW 100 4.12 281 397 561 764
122.20 123.50 1.30 NTW 98 0.427 23.7 0.40% 0.23% 0.31%
256.03 259.08 3.05 NTW 99 0.513 2.29 65 75 306
348.73 351.73 3.00 BTW 99 0.775 5.1 11 434 74
LB-DDH-002 -45 65.50 68.60 3.05 NTW 100 0.257 17.4 138 505 415
73.15 76.20 3.05 NTW 100 1.067 5 161 96 309
82.30 83.80 1.50 NTW 100 0.188 7 74 362 528
89.21 94.50 5.28 NTW 100 0.186 7.8 305 0.11% 0.11%
107.68 108.60 0.92 NTW 100 0.266 13.7 86 0.13% 0.16%
LB-DDH-003 -45 172.22 173.72 1.50 NTW 97 10.7 516 0.50% 2.54% 2.42%
175.26 176.76 1.50 NTW 98 0.115 7.8 161 0.16% 0.26%
LB-DDH-004 -45 198.40 199.90 1.50 HQ 92 0.295 2.8 31 180 486
199.90 201.35 1.45 HQ 82 0.727 33.8 129 631 881
201.35 202.85 1.50 HQ 89 0.187 11 59 368 912
352.70 355.75 3.05 NTW 97 0.288 1.7 30 44 118
LB-DDH-005 -60 133.95 135.30 1.35 HQ 90 0.169 6.6 331 0.18% 0.33%
152.40 153.93 1.53 NTW 100 1.37 10.7 289 0.27% 0.41%
153.93 155.45 1.52 NTW 100 0.211 11.2 663 0.63% 0.87%
LB-DDH-006 -45 32.00 33.50 1.50 HQ 97 0.203 2.7 19 92 88
48.74 50.29 1.55 HQ 97 0.148 19.1 235 379 462
50.29 51.79 1.50 HQ 93 3.91 110 868 510 413
65.53 67.05 1.52 HQ 98 0.109 32.7 222 612 0.12%
LB-DDH-007 -60 128.59 130.30 1.71 NTW 100 0.015 5.4 971 0.24% 0.36%
251.82 252.98 1.16 NTW 94 0.014 7.5 775 0.56% 0.91%
278.00 279.40 1.40 BTW 98 0.007 4 336 0.47% 1.14%
279.40 281.10 1.70 BTW 100 0.02 6.8 759 0.35% 0.40%
286.51 287.71 1.20 BTW 100 0.015 5.5 411 0.60% 0.56%
hole id dip
from to intercept core rec Au Ag Cu Pb Zn
(m) (m) (m) dia % gpt gptppm or
%
ppm or
%
ppm or
%
LB-DDH-008 -45 134.11 137.16 3.05 HQ 97 0.094 7.6 0.10% 0.19% 0.38%
137.16 138.66 1.50 HQ 95 0.028 7.6 522 0.44% 0.64%
141.71 143.26 1.55 HQ 95 0.035 9.7 699 0.18% 0.22%
143.26 144.76 1.50 HQ 95 0.118 5.2 252 0.14% 780
147.80 149.35 1.55 HQ 98 0.402 6.6 555 0.24% 0.14%
210.31 213.36 3.05 HQ 97 0.237 1.6 42 80 120
213.36 216.41 3.05 HQ 98 0.043 4.7 116 0.13% 0.17%
LB-DDH-009 -60 86.80 89.85 3.05 HQ 99 0.106 5 27 130 283
262.25 263.55 1.30 HQ 100 0.261 8.5 373 0.15% 0.21%
LB-DDH-010 -60 10.64 12.19 1.55 HQ 99 0.123 7.6 27 83 48
19.79 21.34 1.55 HQ 100 0.985 25.8 39 126 66
51.82 54.86 3.04 HQ 98 0.186 1.7 33 69 77
192.02 193.52 1.50 HQ 88 0.014 7.7 19 0.82% 625
288.51 290.06 1.55 NTW 62 0.064 23.6 1.13% 3.69% 6.48%
294.13 297.18 3.05 NTW 98 0.016 2.5 100 375 0.12%
409.85 411.28 1.43 NTW 100 0.136 1.7 7 311 566
LB-DDH-011 -60 51.82 53.32 1.50 NTW 100 0.549 37.8 44 260 458
102.08 103.63 1.55 NTW 93 0.268 1.1 11 49 81
170.69 172.19 1.50 NTW 100 0.121 10.1 437 0.56% 0.47%
181.33 182.88 1.55 NTW 98 0.032 9.7 0.18% 0.28% 0.89%
182.88 183.99 1.11 NTW 97 0.03 23.6 0.42% 0.82% 3.27%
323.08 324.58 1.50 NTW 99 0.036 5.8 22 107 95
LB-DDH-012 -45 38.10 39.60 1.50 HQ 100 1.125 28.9 10 71 54
39.60 41.14 1.54 HQ 100 4.07 75 137 114 49
123.44 124.94 1.50 HQ 100 0.046 4.4 645 648 0.34%
124.94 126.49 1.55 HQ 100 0.088 10.9 0.21% 0.11% 0.39%
126.49 127.99 1.50 HQ 100 0.386 26.4 0.13% 0.22% 0.24%
217.93 219.43 1.50 HQ 99 0.023 2.2 304 624 0.15%
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GUADALUPE Y CALVO CONCLUSIONS
• The Guadalupe y Calvo project area is a famous and highly prospective highgrade gold-silver district in the Sierra Madres.
• The property contains the historic Rosario mine, with historic resourcesestimated by Aurico in the Rosario and Nankin veins of 1.861 milliontonnes indicated, grading 120 gpt silver and 2.4 gpt gold for 7.1 millionounces of silver and 142,000 ounces of gold; plus 0.154 million tonnesinferred grading 94 gpt silver and 2,1 gpt gold for 0.5 million oz silver and11,000 oz gold
• There is strong evidence of mineralization in other areas of the project, mainlyin San Carlos and El Chapito, that have not been drilled.
• Along the Rosario trend, there are another areas that need to be evaluated withmore field work, supported by the large database of the project and theregion, including geology, geochemistry, geophysics and drill core, whichgive a good potential to locate more resources.
• A 20 hole, 5,000 m drill program is recommended to test for bonanza mineralizationalong strike and at depth from the Rosario mine