Mountain Boy Continues to Discover VMS Mineralization on Its Surprise Creek Property
June 26 2019 - 10:55AM
Mountain Boy Minerals Ltd (“Mountain Boy” or the
“Company”) (TSX.V: MTB; Frankfurt: M9UA)
reports that field work by the geological team has produced further
evidence for an extensive silver-lead-zinc Volcanogenic Massive
Sulphide (“VMS”) district on the Company’s Surprise Creek property.
The latest discoveries are 1.6 and 3.4 kilometres north of the
Ataman silver-lead-zinc zone and occur within similar stratigraphy.
Drilling on the Ataman zone in 2017 produced highly encouraging
values of silver-lead-zinc within a barite-rich zone (see news
release January 31, 2018). The 100% owned Surprise Creek property
is 32 kilometres northeast of Stewart located in the “Golden
Triangle” of British Columbia. The Company’s BA property is
adjacent and contiguous to the south of Surprise Creek with Highway
37A passing through the centre of the properties.
Previous work by multiple operators on the
Surprise Creek and BA properties has identified silver-lead-zinc
mineralization over a 20-kilometre-long trend. Drilling on the BA
zone between 2006 and 2010 outlined a large VMS occurrence.
The Company views the Surprise Creek and BA properties as
having district scale potential for silver-lead-zinc as well as
gold-copper.
The two new discoveries feature galena and
sphalerite mineralization; both zones are associated with barite or
quartz veining. One of the zones occurs as sheeted quartz veins
over 250 metres. The second zone occurs in a 50 to100 metre wide
area that appears to be underlying the Salmon River formation.
These newly found occurrences are similar to others in this
emerging district as well as to well-established VMS districts
(Figure 1).
Mountain Boy has engaged Dr. Bruce Gemmell, a
renowned expert in VMS geology, to provide guidance in
understanding this district-scale system. He is presently working
with a recently compiled database. Dr. Gemmell will be visiting the
property in late July to work with the geological team and gather
first-hand data.
VMS style mineralization continues to be found
along this 20-kilometre trend and the retreating glaciers continue
to expose new outcrops. The present work is focused on defining the
prospective ore horizon and developing future drill targets.
Besides the VMS targets, other styles of
mineralization occur on the Surprise Creek and BA properties,
including gold-silver bearing quartz veins and copper-gold zones at
the historic George Copper mine and George Copper West.
The Mountain Boy geological and management team
are also compiling and interpreting more than a century of data on
the American Creek West project. The Company recently consolidated
three large properties covering a highly prospective geological
setting centered on the historic Mountain Boy mine. The Mountain
Boy mine produced high-grade silver into the 1930’s. This
first-ever comprehensive review is leading to an understanding of
this exceptionally rich geological mineral system. Fieldwork will
begin on the American Creek West project in mid-July and is
intended to further enhance the geologic picture and establish
drill targets.
Mountain Boy intends to continue the cooperative
exploration program with Auramex Resource Corp, which holds
properties adjacent to both the Surprise Creek and the American
Creek West projects. Both companies are benefitting enormously from
the sharing of data and interpretations as well as logistical
benefits of working cooperatively on adjoining properties.
The technical disclosure in this release has
been read and approved by Andrew Wilkins, B.Sc., P.Geo., a
qualified person as defined in National Instrument 43-101.
On behalf of the Board of Directors:
Lawrence RoulstonPresident &
CEO(604) 914-2142
For further information, contact: Nancy
CurryVP Corporate
Development
(604)
220-2971
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.
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