Source: The Critical Investor for Streetwise Reports 03/16/2019
The Critical Investor discusses insights management has gleaned from recent drilling and why they have the potential to cause a share re-rating.
It took Avrupa Minerals Ltd. (AVU:TSX.V; AVPMF:OTC; 8AM:FSE) a few weeks longer than anticipated to release the first drill results of the Q4 2018 program on the Sesmarias project, part of its Alvalade license located in Portugal, as bringing good news right before PDAC usually generates healthy attention, but the numbers came out pretty interesting anyway in my view. The self-funded 2018 drill program appears to be a real eye-opener for management, as the recently completed 2,498 meters of drilling (6 holes) not only changed their insights on the position of the mineralized lenses discovered so far, but also showed other potentially mineralized structures by intercepting stockwork besides lenses. Step-out drilling of the known 10 Lens is also going according to plan, adding decent tonnage rapidly. Here is an overview of the identified mineralized envelopes/zones at Sesmarias:
The 10 Horizon as defined on this map from the February 11, 2019, news release has been promoted to the 10 Lens now, as sufficient drill results have been obtained so far. Management also provided investors with a schematic long section in the same news release, which is a conceptual drawing of geology and mineralized bodies:
Highlights from the program include the following results according to the latest March 11, 2019, news release:
- SES026 intercepted 28.95 meters of 0.48% copper, 0.77 g/t gold, 15.7 ppm silver, 0.52% lead and 1.31% zinc, and extended the 10 Lens by 300 meters to the north from previous drilling.
The full table of results of hole SES026 looks like this:
This generates a copper equivalent grade of 1.86% CuEq, which is consistent with the other holes drilled into the 10 Lens, as can be seen here as a reminder:
It is also in line with the average grade of 1.5–1.7% CuEq management is looking for when building tonnage for an eventual deposit at Sesmarias.
- The 10 Lens is now at 600 meters x 300 meters x 25 meters. Mise-à-la-masse (MALM) geophysical anomalism extends another 150 meters past SES026 location.
These dimensions generate 4.5 million cubic meters, which in turn result into 18 million tonnes (Mt), when using a conservative gravity of 4t/cubic meter (m3). Average gravity is estimated by management to be ranging from 4 to 4.4t/m3. Using a midpoint would render 18.9Mt. It is interesting to see that the follow-up downhole survey (MALM) detected a further 150m extension, which hypothetically could bring in another 4Mt if continuous. The minimum economic tonnage target of management is 25Mt, so things are progressing quite nicely so far.
- Discovered a possible new mineralized horizon in SES026, located above the 10 Lens, and intersected it again in SES027 and SES029.
No economic mineralization has been hit there yet, but according to management the drill bit did hit sulfides, so there could be a mineralized envelope very close by. Holes SES026, SES027 and SES029 intersected more specifically a horizon of stockwork quartz-sulfide veining located 20-40 meters above the 10 Lens. While mostly iron sulfides, the location of the horizon suggests potential for another possible mineral layer in the Sesmarias massive sulfide system.
- SES028 intercepted the edge of a significant feeder zone stockwork beneath the 8 Lens. Assays indicated anomalous gold, silver, copper, lead and zinc throughout the entire length of the stockwork from 373.40 meters to 460.80 meters in depth, beneath the 8 Lens.
These assays looked like this, and management interprets them as strong indicators for more mineralization in the direct vicinity, and might be the possible edge of a feeder zone for the previously discovered 8 Lens:
The location of holes SES026, SES027 and SES028 can be found here:
Long section view (looking to the east) of the “2” Lens, “26” Horizon and “10” Lens (in red). Note the large, unexplored area to the left of the 26 Horizon and the 10 Lens. The “8” Lens Area and “9” Horizon are marked with dashed red lines. The Eastern Bounding Fault is the darker blue background.
- Confirmed that the high-grade 2 Lens is a fault-bounded fragment of massive sulfide mineralization with origin yet to be determined. Hole SES003, drilled previously on this target, is now also being assayed and will be reported shortly.
Hole SES003 is located very close to SES002, which showed 10.85 meters @ 1.81% Cu; 75.27 ppm Ag; 2.57% Pb; 4.38% Zn; 0.13% Sn, which is not bad as the average copper equivalent grade is 4.97% CuEq, however the volume of the 2 Lens is still too small to be economic as an underground orebody at some distance of the 10 Lens and 26 Horizon.
- Continued re-logging of historical drill holes has upgraded targets in the northern portions of the Sesmarias Prospect.
- Each hole drilled in this exploration phase of the project has enhanced the revamping of the exploration model. Combined with strong assay results in SES026, in particular, the information will be used in the next drill targeting exercise for this large area.
I will elaborate more on this in a second. First, according to management, the mineralization is open to the east boundary fault (see 3D model below in blue) and to the west intersection of the Devonian host rocks and the Tertiary gravels. The 10 Lens appears to be cut by post-mineral dikes to the north, but remains open to the south, though faulting may truncate (=limit) the lens about 100 meters south of SES021.
Plan view of the “10” Lens, “2” Lens, and “8-9” Lens/Horizon (red) and East Bounding Fault zone (transparent blue).
By revamping the exploration model, management means to describe that the current drill results had a profound impact on the understanding of the structural geology of Sesmarias. It appeared that the stratigraphy (complex of layers), especially the orientation of the various layers and mineralized zones, was different from previously understood. As Sesmarias has a pretty complex geology, with lots of faults, folds and potentially folded folds, it was hard to determine the structural controls of any mineralized zone perpendicular on the strike directions. According to the geologists, this area has been deformed several times in the past 360 million years, so this makes determining the linears (directions in different dimensions) very difficult at times. By simplifying everything to layers (rock material of the same character, which is much easier to visualize than anything else) and then trying to connect the same layer between drill holes, they found it easier to construct a pretty good subsurface geological map.
As it turned out, the orientation of the discovered lenses changed from predominantly sub-vertical to relatively horizontal because of new insights. I wondered how this process actually materialized for the geologists, and had a few follow-up questions as well. Fortunately management went out of their way to provide me with pretty extensive answers and explanations, to make sure yours truly, but also the audience, would understand what the exploration program at Sesmarias is all about. Here we go:
“The change in ‘attitude’ (orientation!) came about because we stepped away from the details of rock layers and re-grouped layers into packages of layers with similar characteristics. We were able to follow packages of layers from drill hole to drill hole, over 100s of meters of distance, and we began to see uniformity of the layers around the area between the bounding fault on the east side of the main Sesmarias target area and the area towards the west where the layer packages are in contact with the tertiary gravels and sediments. When we first saw the rocks, we were quite sure that the thin, well-folded units we observed were really and truly folded layers of rocks. However, now we realize that those folds may not actually be folded layers, but folded structural attributes (meaning more abstract comprehensions like axis or intersections). Basically we probably could not see the forest for the trees.
“So, by following these packages from hole to hole, we (mostly meaning our geo Josh Coder) began to build a geological model using a 3D modeling program called GeoReka. By building the model, we began to see more regularity in the rocks, allowing more predictability in our mineralization. The layers generally dip to the east at 30-45 degrees, and plunge to the north. This means our target appears to dip to the northeast until it is stopped by a high-angle fault, which in-house we call the Joana Fault. The Joana Fault does not run in a straight line, so this is a bit of a complication, but we do know now why some of our holes drilled with both Antofagasta and Colt (previous JV partners) did not hit mineralization.
“For now, this fault is limiting mineralization on its west side. This will hopefully change when we do more drilling east of this particular fault. Right now, we think the rock units/layers have been down-dropped on the east side of the fault, but this is only based on limited information from 2-3 holes drilled further away to the east. One of those holes was our own SES014, which we now think may have been stopped short (we actually thought the same when we drilled it, but we had a lot less knowledge back then). In any case, there is an off-hole geophysical conductor in SES014, which we have described as our eastern basin target.”
As hole SES014 is located quite a bit to the east and away from the big fault, I was wondering why management thought there could be mineralization present, also considering the different rock types over there which usually don’t contain mineralization based on earlier results, despite all potential vertical and lateral displacements. They had this to say:
“When talking about having more chance to the east, we meant just across the fault. There is a chance over there because of the potential downdrop (vertical movement), compared to the west side of the fault. That means the target rocks/layers are deeper, though certainly possibility of horizontal movement exists, as well.”
Again as a reminder, Sesmarias contains a large amount of faults and off-setting structures, constructing an interesting puzzle from a geological standpoint:
Management elaborates further on their exploration plan:
“The re-interpretation of the orientation of layers gives us a lot of license to re-orient the mineralization, as it is basically just another bed/layer. SES026 targeted the “extension” of the layer, successfully intersecting massive sulfide mineralization. SES027 was less successful, as it intersected weak mineralization and mafic intrusive rocks, which may represent the source of the mineralization. We are thinking that the mafic rocks represent part of an intrusional dome, right now with known mineralization to the south of it. We do not know yet if there is further mineralization on the north side of the dome, as portrayed in the long section further below.
“So we estimate a potential strike length of somewhere between 600 and 900 meters of massive sulfide mineralization, which stops somewhere between holes 26 and 27. The new, more horizontal positioning of the massive sulfide allows for a much bigger target at shallower depth, where the more vertical positioning gives a target of the same shape, but gets very deep, very quickly.”
Therefore I view this adjusted orientation as a positive, as it saves drilling budget. On my question if cross sections could be provided anytime soon, management answered they needed some more drilling in order to get sufficient understanding of continuity. They added:
“Right now, 2, 8, and 26 are more horizons than actual masses, and presumably smaller than the 10 Lens. Horizon 2 appears to be small, though high grade (SES002), and it is open to the south. We have seen traces of Horizon 26 in 3-4 holes now, and it is presently manifested by strong stockwork to semi-massive sulfide material. We think that there is a possibility that Horizon 8 could be an extension of the 10 Lens, because it is roughly at same depth, and horizontal displacement of surrounding packages through faults checks out with this concept. Horizon 8 could have its own feeder source as it is on the other side of this basalt dome, as both Horizon 8 and the 10 Lens are roughly parallel to each other and to stratigraphy. More drilling is necessary to figure this all out.”
Looking at the schematic long section again, I noticed that 025 and 027 missed the massive sulphide lenses. It made me wonder if by more vertical faulting/displacements there could be (off set) extensions of the lenses/horizons, or these basalt domes could be structurally consistent and not broken up/displaced by faults, limiting mineralized potential in these areas except for stockwork (027)? To what extent could this stockwork be useful/economic? Management had this to say:
“SES025 ‘hit’ the 2 Lens at predicted depth, but it was very thin (