The airborne survey is awaiting final approval of the proposed flight
path and area to be surveyed from the government department of Civil
Aviation. The survey will commence within 3 weeks of the receipt of the
permit. It will encompass all of the Company's western permits and the
favourable stratigraphic horizons within the southwestern portion of the
Troodos complex.
Based on a compilation of the previously completed drilling and the
results of the ongoing surface exploration the Company believes that the
Anglesides – St. Nik style of mineralization, which is significantly
enriched in precious metals, represents a late or waning stage of the
hydrothermal system that operated throughout the period of volcanism in
Cyprus. The correlation of these two high grade showings with the volcanic
– sedimentary contact provides a new target for further exploration on the
island.
Northern Lion continues to collect rock and soil samples over known
gossan zones and this work has been expanded to include those areas
believed to have potential for the St. Nik style mineralization. This work
has already identified a new St. Nik style showing which has been covered
by the Company's latest permit application. These ground based geochemical
surveys in conjunction with the airborne geophysical survey are expected
to generate additional drill prospect targets for the rotary program. The
rotary drill is a quick and extremely cost efficient prospecting tool
which will aid in outlining the lateral extent and the level of
mineralization of buried targets. Rotary holes are initially planned to
test additional targets in the Anglesides area, and to evaluate the
potential extensions of the St. Nik mineralization beneath the sedimentary
cover.
The results from the 2011 Diamond drill program on the Pitha,
Anglesides and Asproyia projects, are discussed below. The overall drill
program totaled 2,863.2m in 32 holes which tested 5 separate targets as
shown in the following table.
|
Holes |
|
Project |
Drilled |
Meters
Drilled |
Pitha |
7 |
938.6 |
Anglesides |
6 |
384.6 |
St.
Nik |
7 |
541.1 |
Asproyia |
7 |
576.8 |
Evoloimeni |
5 |
422.1 |
Results of the St. Nik and Evoloimeni drilling were previously released
April 6, 2011 and June 29, 2011 and returned 4.5 g/t gold over 28.6 meters
and 1.3 g/t gold over 24.3 meters respectively.
Pitha Project
At the Pitha project, the drill program was designed to follow-up on
the 2010 results and test geochemical and geophysical Induced Polarization
(IP) targets. A single hole (11PT03) was drilled within the pre-existing
cut to test for a possible extension of the massive sulphide zone
encountered in a hole drilled in 2010 (10PT02), which returned 4.9 meters
of 5.1% copper and 0.2 g/t gold within a larger interval of 38.9 meters of
0.8% copper and 0.2 g/t gold (see news release September 29, 2010). Narrow
intercepts of massive pyrite were encountered with minor copper and zinc
values. Holes 11PT04, 05 and 06 tested IP targets with coincident
geochemical anomalies in the southern portion of the property. In 11PT04 a
33.8m zone contained anomalous gold and silver mineralization starting
near surface and correlates with surface rock samples containing up to
2g/t gold. Sporadic gold values were intersected along with stringer type
copper mineralization in holes 11PT05 and 06. These intercepts occur
within the Basal Group rocks.
Hole 11PT07 tested a strong IP chargeability anomaly in Lower Pillow
Lavas associated with a weak soil anomaly 400m north of the cut area.
Abundant disseminated to stringer type pyrite mineralization was
encountered with minor gold, copper and zinc values. Holes 11PT08 and 09
targeted a combined IP chargeability and zinc-gold soil geochemical
anomaly within the Upper Pillow Lava series. Strongly altered pillow lavas
were encountered in 11PT08 with weakly anomalous gold values. Drill hole
11PT09 intersected a major northerly trending structure carrying anomalous
values in gold, silver copper and zinc over a width of 29.9m. Within this
large structure a narrower zone of 9.6m contained elevated gold, silver
and zinc values that correlate with a zone of surface gossans.
Pitha - Significant assay drill results: |
|
|
|
|
|
|
|
|
|
From |
To |
Interval |
Au |
Ag |
Cu |
Zn |
Hole # |
(m) |
(m) |
(m) |
g/t |
g/t |
% |
% |
11PT03 |
6.6 |
86.6 |
80.0 |
0.15 |
1.1 |
0.1 |
0.11 |
|
incl |
6.6 |
40.6 |
34.0 |
0.19 |
1.0 |
0.21 |
0.22 |
|
incl |
6.6 |
26.5 |
19.9 |
0.16 |
0.96 |
0.24 |
0.34 |
11PT04 |
22 |
55.8 |
33.8 |
0.24 |
1.48 |
0.23 |
0.17 |
11PT09 |
37 |
66.9 |
29.9 |
0.28 |
3.9 |
0.08 |
0.5 |
|
incl |
37 |
46.6 |
9.6 |
0.74 |
9.2 |
0.02 |
1.1 |
Angelsides
Project
At Anglesides a series of 6 holes were desigined to test several target
types; the area immediately surrounding the surface rock sampling, a
strong IP resistivity anomaly located southwest of the surface sampling,
and a weak IP chargeability high to the east. Anomalous gold values up to
2.36g/t over 0.5m was intersected in holes 11AN01 to 03, however the high
grade values from the surface rock sampling was not repeated. Two samples
in hole 11AN03 returned very high silver grades of up to 585g/t over 1.8m.
It is hypothesized that the gulley tested by the surface sampling may
represent an ancient open pit mined by the Romans. The material sampled by
the Northern Lion field crew, including 10 meters of 6.6 g/t gold, (News
Release September 15, 2010) is now thought to be the material that was
left behind on the walls of the excavation, after Romans had removed the
high grade massive sulphides.
The grade and location of the mineralization within the stratigriaphic
section at Anglesides is similar to the mineralization found at St.
Nikolas. In both locations there are unweathered and silicified massive
sulphides at or close to the contact with the overlying sedimentary
sequence. Follow-up work at Anglesides will focus on testing this Upper
Pillow Lavas – Sediment contact zone.
Angelsides - Significant assay drill results: |
|
|
|
|
|
|
|
|
|
From |
To |
Interval |
Au |
Ag |
Cu |
Zn |
Hole # |
(m) |
(m) |
(m) |
g/t |
g/t |
% |
% |
11AN01 |
0 |
8.1 |
8.1 |
0.4 |
3.0 |
0.36 |
0.26 |
|
incl |
2.6 |
9.8 |
7.2 |
0.39 |
3.0 |
0.47 |
0.19 |
11AN02 |
0 |
33.8 |
33.8 |
0.37 |
2.3 |
0.33 |
0.16 |
|
incl |
0 |
12.6 |
12.6 |
0.5 |
3.7 |
0.55 |
0.34 |
11AN03 |
2.5 |
33.4 |
30.9 |
0.34 |
37.0 |
0.35 |
0.02 |
|
incl |
2.5 |
20.1 |
17.6 |
0.49 |
65.1 |
0.47 |
0.03 |
|
incl |
4.4 |
6.8 |
2.4 |
0.54 |
448.0 |
0.61 |
0.03 |
Asproyia
Project
The Asproyia property was tested by 7 holes targeting a combination of
geochemical and IP geophysical targets. The majority of the Asproyia grid
area is underlain by Basal Group rocks and the style of mineralization
encountered in the drilling reflects this environment. Chalcopyrite filled
fractures and stringers up to 1cm wide were intersected in all holes.
Drill hole 11AS02 returned 0.57% copper over a 49.7m interval. This
mineralization is believed to represent a feeder system to a mineralized
zone higher in the stratigraphic section and has subsequently been removed
by erosion.
Asproyia - Significant assay drill results: |
|
|
|
|
|
|
|
|
|
From |
To |
Interval |
Au |
Ag |
Cu |
Zn |
Hole # |
(m) |
(m) |
(m) |
g/t |
g/t |
% |
% |
11AS01 |
3 |
38.8 |
35.8 |
0.03 |
0.1 |
0.4 |
0.02 |
11AS02 |
4.5 |
80.1 |
75.6 |
0.02 |
1 |
0.42 |
0.01 |
|
incl |
24.6 |
74.3 |
49.7 |
0.02 |
1 |
0.57 |
0.01 |
11AS05 |
20.2 |
22.5 |
2.3 |
0.02 |
0.3 |
1.27 |
0.01 |
11AS07 |
48.9 |
100 |
51.1 |
0.01 |
0.1 |
0.37 |
0.01 |
History
The history of mineral exploitation (copper, gold and other metals) on
the island of Cyprus dates back to the Bronze Age, approximately 5,000
years ago. The Phoenicians were the first to process copper on the island,
followed by the Romans and this activity has continued to the present day.
The evidence of this long history of mining is readily observed in the
abundant ancient surface and underground workings along with extensive
slag heaps. Mineral exploration in the Republic of Cyprus has been at a
very low level over the last few decades, and management believes that
there is a high probability of additional massive sulphide bodies being
present that did not outcrop, as nearly all of the known deposits did.
The metal deposits of Cyprus are dominantly copper-bearing volcanogenic
hosted massive sulphide "VHMS" deposits. These deposits are hosted within
the pillow lava sequence of the Troodos Ophiolite Complex.
Quality Control
and Assurance
The Company's field activities in Cyprus are under the direction of Jim
Chapman, P.Geo. (BC), consultant to the Company and "qualified person", as
defined by National Instrument 43-101, who is responsible for the
technical content of this news release.
About Northern
Lion
Northern Lion Gold Corp. is a Canadian mineral exploration company,
listed on the TSX Venture Exchange and the Frankfurt Exchange. The Company
is committed to building a strong portfolio of projects within
mining-friendly and infrastructure-rich areas of Europe.
In addition to its exploration permits in Cyprus, the Company holds a
100% interest in its Moura Licence in Portugal and a 100% interest in one
project in the historic Bergslagen mining district of southern Sweden.
NORTHERN LION GOLD CORP.
John Lando, President