Omai Gold Mines Corp. (TSX VENTURE:OMG) ("Omai" or the "Company")
is pleased to announce the first results from an ongoing program of
logging and sampling of 6,000 meters of unassayed core from a 2012
drilling program that had been preserved by the Guyana Geology
& Mines Commission (GGMC). The assay results from the first two
of these holes,
12WED11 and
12WED13, which were never logged or sampled,
indicate that high-grade mineralization extends below the Wenot Pit
and there is expansion potential of gold mineralization to new
sedimentary targets.
Highlights of the assay results:
- Hole
12WED11 intersected intervals such as 20.6 meters of 3.55
grams per tonne (g/t) gold (Au) from 460 to 480.6 meters,
including 4.5 meters of 8.02 g/t Au, and 10.5 meters of
3.93 g/t Au from 400.5 to 411 meters (see Table 1 below
for full results).
- Visible
gold was encountered in hole 12WED11. Highest assay values include
29.19 g/t Au over 1 meter from 460 to 461 meters.
- Hole
12WED13 intersected 4.5 meters of 2.93 g/t Au from
54 to 58.5 meters to the south of the Wenot Pit in sedimentary
rocks, where there has been no previous exploration and may be
vectoring towards a second mineralized “Wenot style system.”
-
The results in hole 12WED11 extend gold mineralization at least 150
meters below the bottom of the Wenot Pit (see Figure 2) and
mineralization remains robust at this depth with no indication of
decreasing.
Mario Stifano, Chief Executive Officer of Omai
Gold Mines, commented: “We are very pleased that the results from
these two holes confirm that high-grade gold continues beyond the
limits of the Wenot shear and the Wenot Pit to the south within the
sedimentary package, and that mineralization from the Wenot Pit
continues at least 150 meters below the depth of the historical pit
that was mined. These results support our planned initial
5,000-meter drill program beginning in the new year.”
Table 1: Intercepts in holes 12WED11 and
12WED13.
Hole number |
Depth from (m) |
Depth to (m) |
Interval (m) |
Au (g/t) |
12WED11 |
372 |
380 |
8 |
1.21 |
|
382 |
385.5 |
3.5 |
0.39 |
|
400.5 |
411 |
10.5 |
3.93 |
|
413 |
419.4 |
6.4 |
0.77 |
|
436 |
438 |
2 |
4.65 |
|
440.1 |
442.1 |
2 |
7.69 |
|
460 |
480.6 |
20.6 |
3.55 |
including |
460 |
464.5 |
4.5 |
8.02 |
12WED13 |
54 |
58.5 |
4.5 |
2.31 |
Note: A 0.3 g/t cut-off and internal dilution of
up to 4 meters of continuous internal dilution were used. Some
intervals are shorter due to missing core boxes. Widths are
reported as downhole width. True widths may be related to near
vertical structures, but with tension veins, this cannot be
assumed.
Table 2: Highest intervals in 12WED11
include:
Depth from (m) |
Depth to (m) |
Au (g/t) |
460 |
461 |
29.19 |
472.2 |
472.9 |
27.45 |
406.5 |
407.5 |
21.97 |
441.1 |
442.1 |
13.90 |
436 |
437 |
8.82 |
404.5 |
405.5 |
5.88 |
477.8 |
478.8 |
5.21 |
372 |
373 |
4.96 |
405.5 |
406.5 |
4.93 |
Of the two holes reported here, hole 12WED11 was
drilled toward the north under the Wenot Pit (see figures 1 and 2)
and encountered high-grade gold associated with the Wenot shear,
whereas hole 12WED13 was drilled to the south into folded and
sheared sedimentary rocks south of the Wenot shear zone (see Figure
1).
Gold mineralization in hole 12WED11 occurs in
and around quartz-ankerite extensional veins within an alteration
assemblage of strong silica-ankerite-sericite. Lithicwacke
sedimentary units that are sheared and cut by quartz diorite dikes
host mineralization. The dikes increase in frequency more proximal
to the Wenot shear zone. The Wenot shear is a wide zone of intense
subvertical dextral shearing, including proto mylonite that
reflects the intensity of deformation, along the contact between
the mineralized sedimentary rocks to the south and the mineralized
basalts and andesites to the north. Due to missing core boxes for
hole 12WED11 the a proto mylonite was not observed, however proto
mylonite is observed in other holes currently being logged and
sampled. The intensity of structural deformation and the presence
of felsic dikes indicate that the Wenot shear taps underlying
felsic intrusives for ore fluids.
In hole 12WED13, no significant assays were
expected, but one sample contained 6.6 grams and the duplicate
sample collected as part of standard QA/QC returned a value of 50
grams of gold. This interval is a weathered quartz vein in
saprolite below unmineralized younger sands. Because of the
weathering and location just below sand cover, the gold content is
variable due to a nugget effect related to weathering. In hole
12WED13, shear and tension veins are filled with
quartz-calcite-ankerite veining and some anomalous gold
mineralization. Quartz diorite dikes increase in thickness and
abundance to the south and may reflect proximity to another
mineralizing system like Wenot.
Figure 1: Plan map of Omai showing holes
12WED11 and
12WED13.https://www.globenewswire.com/NewsRoom/AttachmentNg/0b4c3bab-b9f4-4fa0-80c1-d9e40b64e4d8
Figure 2: Cross section of hole
12WED11.https://www.globenewswire.com/NewsRoom/AttachmentNg/b15a4f7a-d12c-4246-812c-64b7a9231785
Sample collection, assaying and data
management
Core samples were collected at 1 to 2 meter
intervals and represent ½ of whole NX size core. Standards, blanks
and duplicates were entered at regular intervals. Samples were
sealed in plastic bags and shipped to the Actlabs certified
laboratory in Georgetown, Guyana, respecting the best chain of
custody practices. At the laboratory, samples were dried, crushed
up to 80% passing 2 mm, riffle split (250 g), and pulverized to 95%
passing 105 μm, including cleaner sand. 30 g of pulverized material
was then fire assayed by atomic absorption (AA). Initial assays
with results above 3,000 ppb gold are re-assayed with gravimetric
finish. Assay data is subject to QA/QC. For hole 12WED11, pulps
from mineralized intervals were sent to MSALABS in Georgetown for
confirmation analyses. Results show a 94 percent correlation and if
one high-grade sample with coarse gold is excluded, a 99 percent
correlation. Assays of new pulps prepared from rejects by ACTLABS
confirm the same correlation of 99 percent.Table 3: Drill
coordinates and orientation.
Hole number |
Eastings |
Northings |
Elevation |
Max depth |
Dip |
Azimuth |
12WED11 |
304903 |
601316 |
52.1 |
535 |
-50 |
0 |
12WED13 |
305500 |
601254 |
43.1 |
454.6 |
-50 |
180 |
Note: Coordinates PSAD56 Zone 21N.
Qualified Person
Dr. Dennis LaPoint, PhD, LGeo, is a Qualified
Person (QP) under National Instrument 43-101 "Standards of
Disclosure for Mineral Projects" and has approved the technical
information contained in this news release. Dr. LaPoint is not
considered to be independent for the purposes of National
Instrument 43-101.
Neither the TSX Venture Exchange nor its
Regulation Services Provider (as that term is defined in the
policies of the TSX Venture Exchange) accepts responsibility for
the adequacy or accuracy of this release.
About Omai Gold Mines Corp.
Early prospectors identified Guyana’s vast
mineral wealth 130 years ago, and at the heart of the country’s
gold mining history is the Omai mine: a multi million-ounce deposit
that was once South America’s largest producing gold mine. We’re
building on this past success with new tools, relationships and
vision to bring this under-explored gold district back to life,
providing a unique opportunity for all stakeholders to participate
in value creation.
Avalon Gold Exploration Inc., a wholly owned
subsidiary of Omai Gold Mines Corp., holds a 100% interest in the
Omai Prospecting License covering 4,590 acres, including the past
producing Omai gold mine.
For further information, please see our website
www.omaigoldmines.com or contact:Mario
StifanoPresident and Chief Executive
Officerinfo@omaigoldmines.com
Cautionary Note Regarding Forward-Looking Statements
This news release includes certain
“forward-looking statements” under applicable Canadian securities
legislation. Forward-looking statements include, but are not
limited to, statements with respect to timing and results of the
drill program. Forward-looking statements are necessarily based
upon a number of estimates and assumptions that, while considered
reasonable, are subject to known and unknown risks, uncertainties
and other factors which may cause the actual results and future
events to differ materially from those expressed or implied by such
forward-looking statements. Such factors include, but are not
limited to: general business, economic, competitive, political and
social uncertainties; delay or failure to receive regulatory
approvals; the price of gold and copper; and the results of current
exploration. There can be no assurance that such statements will
prove to be accurate, as actual results and future events could
differ materially from those anticipated in such statements.
Accordingly, readers should not place undue reliance on
forward-looking statements. The Company disclaims any intention or
obligation to update or revise any forward-looking statements,
whether as a result of new information, future events or otherwise,
except as required by law.
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