BB's Stock Haven

[Skiluc]

ACRL. Strictly Gold and Geographic DD.

Let’s go over some RECENT Studies shall we?

The new discoveries in the South Mine Complex (SMC) generally are of a different style of mineralization with wide sulphide systems rather than the quartz vein mineralization that is found in the Main Break complex. Tellurides appear to be more prevalent in the SMC, compared to the historical mineralized systems, in particular the occurrence of the gold telluride mineral calaverite

From 43-101 dated April 2019 from Kirkland Lake:

https://s21.q4cdn.com/967674075/files/doc_downloads/technical_reports/2019/Macassa-Property-Ontario-Canada-Updated-NI-43-101-Technical-Report-Apr-1-2019.pdf

Several strong northeasterly trending cross-faults offset the mine host rocks and mineralized zones with displacement usually to the south (dextral) and up on the west side. Major cross faults are the Lakeshore Cross Fault near the east end,... and the Amikougami Creek fault at the west end of the mine.

Left is Amikougami and right is LakeShore. We are right at the wedge. V is for Victory. Green is our Claims:


More studies? Ok:

The Allsopp--Huston property, consisting of 12 leased mining claims, is located 10 km
southwest of Kirkland Lake in Eby and Otto townships. The property has a long history of exploration, dating back to the 1930's, and includes detailed geological mapping, trenching, magnetometer, and IP surveys, diamond drilling and development of a 32 m deep shaft. A major altered deformation zone, consisting of iron carbonate, silicification and pyritization, occurs over a strike length of 1000 m and a width of 200 m on the property along the Eby--Otto fault. This fault is a subsidiary of the Larder Lake Break within Archean tholeiitic metavolcanic rocks. A silicified breccia zone with disseminated pyrite is hosted within the altered deformation zone. The breccia zone has a strike length of 600 m and a width of 50 m. Geochemically anomalous gold values, ranging up to 1851 ppb Au, occur in the breccia zone and the alteration zone. Moderate to strong IP (chargeability) anomalies occur within the alteration zone over a strike length of 800 m and a width of 100 m. The IP anomalies in the alteration zone along the Eby--Otto fault, 1.5 km south of the Larder Break, are attractive targets for further exploration.

http://www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/20000014314/2_56212_10_TechnicalReport.pdf

More? Okay:

At the new South Mine complex, which lays about 300 to 600 meters south of the Main
Breaks, an entirely new mineralized system in the Kirkland Lake mining camp is being mined. It is
characterized by generally shallowly dipping (25°-50°) structurally controlled zones of finely
disseminated pyrite, visible gold and tellurides

These much flatter zones are interpreted to be a "cross over" type faulting passing
between the break series of faults and a as of yet unknown southernly fault system, possibly
directly related to the LCDZ which does also occur to the south

http://www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/20000014634/2_56940_10_Technical_Report.PDF

Let me help make a connection here folks.

“Arnold Allsop” study says that we are 1.5km south of Larder Lake break.

A Kirkland Lake study says 300-600 meters south is the bonanza intercepts with unknown southern fault system.

1.5Km - 600 meters = 900 meters.

900 meters away from 4,750 g/t gold bonanza intercept.

Fact.

I’m embarrassed I didn’t catch that earlier!

900 meters and the southern mineralization is unknown.

I’m betting the gold made the 900 M trip down the same fault!!!!


More? Sure.

Larder - Cadillac Deformation Zone (LCDZ), a major east-west structural control on gold bearing alteration and mineralization, which in much of its length coincides with a folded and deformed sinuous belt of sedimentary rocks of conglomerate, sandstone and volcanic tuffs. The LCDZ is a carbonatized shear zone characterized in some places by the presence of quartz stockwork, and green mica. It is considered to be the western extension of the Malartic-Cadillac Deformation Zone, a more than 160 km long. The deformation zone is a south-dipping reverse fault, the south side of which seems to have moved upward and eastward relative to the north side

Oopsie another technical study link. Sheesh.: http://www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/20000014311/2_56860_10_Technical_Report.PDF

And all the Exploration Permits good for 3 years!!!



How about some maps. Use Hwy 112 as a guide. Rivers help too. Just gonna lay them all out:











Find much more shared DD on posts at: https://investorshub.advfn.com/Atacama-Resources-International-Inc-ACRL-31214/