The Covas property is located in the northwestern corner of Portugal. Tungsten mineralization is contained in a 3 km x 2 km ring of pyrrhotite-bearing skarn deposits surrounding a presumed buried multiple-intrusion complex. Some of the deposits were previously exploited by two Portuguese companies between 1949 and the early 1980’s. Union Carbide and several other companies explored the district extensively up through the mid-1980’s, resulting in approximately 27,000 meters of drilling in 329 holes. However, exploration was not systematic, and only an estimated 40% of the skarn zone was drilled. The central intrusion complex was not at all explored, and there remains a potentially large, bulk-tonnage porphyry tungsten target inside the skarn ring. From the reported drilling, surface trenching, and geological mapping, Union Carbide calculated a mineral resource (non NI 43-101 compliant) of 922,900 metric tonnes of 0.78% WO3 (tungsten trioxide) in the skarn deposits.

CJV Exploration
View CJV Exploration May 2016 Presentation

Recon geochemistry
Avrupa completed a basic geochemical study of the central zone. Analytical results from the 300-sample grid soil survey over the granitic intrusion complex, called the Covas Dome, were positive for tungsten, gold, arsenic, bismuth, and other metals. These results generally defined areas of immediate further interest within the Covas Dome, as shown by the following anomaly maps (Figures 1 through 6). Note that the better tungsten values occur in the SE half of the Dome, while gold is more preferential to the west and west-central portions of the dome. Strong arsenic anomalies are related spatially to both gold and tungsten, and bismuth anomalies are more closely related to areas of anomalous tungsten. Weak molybdenum anomalies cover the entire dome area, and weak tellurium anomalies occupy the central portions of the Covas Dome, partially coincident with the gold anomalies. The geochemical signature indicates potential for further tungsten mineralization, and also the possibility for reduced intrusion-related gold mineralization.

Figure 1. Tungsten in soil anomalies


Figure 2. Gold in soil anomalies


Figure 3. Arsenic in soil anomalies


Figure 4. Bismuth in soil anomalies


Figure 5. Molybdenum in soil anomalies


Figure 6. Tellurium in soil anomalies


Recon geophysics and geological mapping
A predecessor company to Avrupa completed a prospect-wide grid magnetic survey in 2009-2010. Avrupa decided to re-process that data with the idea to better define the shapes of the potential skarn targets, as well as to better define structural controls to mineralization. The following two maps illustrate possible structural controls to mineralization, as well as the relation of magnetic highs around the skarn ring to already-known tungsten skarn deposits. In Figure 7, the tungsten soil anomaly in the Covas Dome is spatially related to a zone of strong magnetism, and known tungsten mineralization in the Skarn Ring is clearly spatially related to strong magnetic highs. However, anomalous gold in soils in Figure 8 is more closely related to strong east-west linears and general magnetic lows. Previously, the presence of gold in the Covas system had not been recognized. However, now it appears that there may be potential for both gold and tungsten mineralization in the Covas Dome area.

The company is now in process of field follow-up of the anomalies and definitive drill targeting in the Dome area, as well as selective targeting in the Skarn Ring zone. Previous mapping and prospecting in 2009 defined some relationships between structures, alteration, and possibility of mineralization. Field studies are presently building on that initial mapping and the recently-completed geochemistry and geophysics work. Avrupa expects to consolidate and prioritize drill targets before the end of the second quarter, in anticipation of first-pass scout drilling during the fourth quarter of 2011.

Figure 7. Residual magentics with tungsten in soils. Note the relationship between known tungsten deposits and magnetic highs in the Skarn Ring, as well as the relationship of the general tungsten in soils anomaly with a strong magnetic high in the Covas Dome area.
Figure 8. Residual magnetics with gold in soils. Note that the better gold values are more closely related to magnetic lows and to two east-west linears, located in the center of the dome area, that define a strong magnetic low.