Vela Minerals Completes Initial Surface Exploration Program at Mavis Bank Jamaica
26 Giugno 2013 - 5:12PM
Access Wire
Vancouver, B.C., Canada, June 26 2013 - Vela
Minerals Ltd. (TSX-V: VLA) (the "Company") is
pleased to announce the results of a recent exploration program on
its Mavis Bank special exclusive prospecting License (SEPL) in
Jamaica. The ground exploration program
consisted of geological mapping, collection of 501 soil samples on
two grids, 84 regional stream samples, and 143 rock samples. Soil
grids for both Mavis Bank and Epping were established in order to
determine the distribution of base, precious, and pathfinder
elements.
Mavis Bank Soil Grid: Sampling results on the Mavis Bank grid feature gold in soil
anomalies on the northwest portion which correlate directly with
strong copper soil anomalies. Additionally, two soil samples taken
in the south portion of the Mavis Bank soil grid area returned 1420
and 1480 ppb Au along with 11.3 and 12.1 ppm Ag, and 6020 and 6200
ppm As respectively. This Au-Ag-As soil anomaly coincides with the
location of a geophysical survey residual gravity anomaly that is
adjacent to several Pulse-EM geophysical survey conductors that
have been interpreted to dip to the west towards the Au-Ag-As soil
anomaly. The Au-Ag-As soil anomaly occurs adjacent to a northeast
trending creek gully and appears to be structurally
related.
Epping Soil Grid: The
Epping grid returned highly anomalous values of 380 to 2010 ppm
copper in soils coincident with anomalous gold values of 10 to 166
ppb Au in four different north-northwest trending lineaments. These
zones of structural weakness roughly coincide with major fault
zones characterized by widespread and locally intense argillic
alteration, silicification, chlorite, and carbonate alteration.
Although the general trend of mineralization is north-northwest,
there is an east-northeast component to the local fabric, which is
reflected in the local east-northeast trend of creek gullies where
the highest copper in soil anomalies occur (14 soil samples ranging
from 338-922 ppm Cu.
Mavis Bank Rock Samples:
Copper is highly anomalous in the Mavis Bank area with most samples
returning between 429 ppm Cu and 9150 ppm Cu. Thirteen
samples returned high-grade copper values of
1.46% - 12.5%. Rock sample number 931383 contains 5.28% Cu, 48.6
g/t Ag, 179 ppb Au, 1900 ppm Co, and 5870 ppm As. The high copper
values obtained from the area are due to the presence of
chalcopyrite and/or malachite, with lesser amounts of chalcocite
and/or azurite, and trace amounts of bornite mineralization
associated with iron oxide and sulphides (pyrite, magnetite,
hematite and specularite). Gold values range from 10 ppb to 301 ppb
Au and correlate with high copper values. Silver values range from
trace to 48.6 g/t and correlate with high copper and gold
values.
Epping Rock Samples: Of the
sixty-four samples taken in this area, thirty-three samples
returned between 585 ppm and 8550 ppm Cu, and ten samples returned
high-grade copper values of 1.52% - 13.7%. Six of these samples are
located in the southwest portion of the grid area and correlate
with anomalous gold values of up to 733 ppb Au, and silver values
of up to 9.42 ppm.. Anomalous silver values are associated with
malachite, chalcocite, chalcopyrite, and bornite
mineralization.
Barbeque River: Limited
sampling was performed in a 300 X 500 meter area elongated
east-west in the Phillip's Gully Area. Of the 21 samples taken,
eight samples graded between 1.14% - 3.15% Cu with a strong
correlation between copper, silver (up to 6.66 ppm), and arsenic
(up to 1770 ppb).
Mavis Bank Regional Setting:
The Mavis Bank Area
possesses similarities to the Pueblo Viejo area of the Dominican
Republic (approx. 25m oz/Au). Structurally complex overprinting of
intrusion related hydrothermal mineralization superimposed on
sedimentary and volcanic host rock with widespread alteration is
present, and the widespread occurrence of Fe-oxides
(magnetite-hematite) associated with Cu-Ag-Au bearing
mineralization suggests potential for Pueblo Viejo style epithermal
precious-base metal deposits.
Technical information in this news
release has been reviewed by Derrick Strickland P.Geo., a qualified
person as defined in NI 43-101.
ON BEHALF OF THE
BOARD OF DIRECTORS
"Derrick Strickland P.Geo."
President
For further
information please contact:
Telephone:
604.773.0992
Email:
info@velaminerals.com
Suite 910 - 475
Howe Street, Vancouver, BC V6C 2B3, Tel 604.773.0992;
www.velaminerals.com
Neither 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.
Cautionary Note
Regarding Forward-Looking Information
This press release contains certain
forward-looking statementswithin the meaning of the Canadian securities
laws, which are based on
the opinions and estimates of management at the date the statements
are made, and are subject to a variety of risks and uncertainties
and other factors that could cause actual events or results to
differ materially from those projected. Forward-looking information
in this press release includes statements about the potential
existence and size of mineralization at the Epping Farm and Mavis
Bank areas, geological interpretations and potential mineral
recovery processes. Information concerning mineral reserve and
resource estimates also may be deemed to be forward-looking
information in that it reflects a prediction of the mineralization
that would be encountered if a mineral deposit were developed and
mined.
In
connection with the forward-looking information contained in this
news release, the Company has made numerous assumptions, regarding,
among other things: the geological, metallurgical, engineering,
financial and economic advice that the Company has received is
reliable, and is based upon practices and methodologies which are
consistent with industry standards. While the Company considers
these assumptions to be reasonable, these assumptions are
inherently subject to significant uncertainties and contingencies.
Additionally, there are known and unknown risk factors which could
cause the Company's actual results, performance or achievements to
be materially different from any future results, performance or
achievements expressed or implied by the forward-looking
information contained herein. Known risk factors include, among
others: the actual mineralization may not be as favorable as
suggested, or at all; uncertainties relating to interpretation of
drill results and the geology, continuity and grade of mineral
deposits; and uncertainty as to timely availability of permits and
other governmental approvals.
Vela undertakes no obligation to update
forward-looking statements if circumstances or management's
estimates or opinions should change. The reader is cautioned not to
place undue reliance on forward-looking
statements.
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