Papuan Precious Metals Corporation: Exploration of Au/Cu Porphyry Potential Commences at Elang Area, New Hanover
28 Giugno 2011 - 2:45PM
Marketwired
PAPUAN PRECIOUS METALS CORPORATION ("PPM" or the "Company") (TSX
VENTURE: PAU)(TSX VENTURE: PAU.WT)(OTCQX: PAUFF) announces that it
has received the interpretation report for the recently completed
New Hanover airborne geophysical survey. A discrete reverse dipolar
magnetic target in the Elang Creek area of EL 1566 New Hanover is
interpreted as evidence for an intrusive different from others in
the project area
http://www.ppmpng.com/New%20Hanover%20geochemical%20anomalies.pdf.
The Elang geophysical anomaly is rated as high priority for
followup by PPM's consulting geophysicists.
The Elang geophysical anomaly is coincident with the 2.5km2
Elang geochemical anomaly
(http://www.ppmpng.com/New%20Hanover%20geochemical%20anomalies.pdf).
Panned concentrate samples collected during March 2009 from streams
draining the area contained anomalous gold (Au greater than 30
microgram) and several rock float and outcrop samples contained
greater than 0.1 g/t Au. These geochemical anomalies were observed
to be coincident with abundant boulders/sub-outcrop of vuggy
silica-breccia and alunite along ridgelines. Followup outcrop
sampling and mapping in May 2010 located copper in an outcropping
6m wide brecciated quartz-sulphide vein (3m @ 0.36% Cu; grab of
selvage @ 0.15% Cu, 20g/t Ag) and extensive zones of silica breccia
alteration and argillization. The Elang anomaly is localized at the
intersection of a prominent west-northwest fault zone and northeast
trending faults, both very obvious from the results of the airborne
geophysical survey.
Coincidence of copper and gold values in outcrop with extensive
zones of argillization and silica breccia alteration and a discrete
magnetic anomaly, localized at the intersection of dominant
through-going structures, is interpreted by the Company to
represent a high priority target for Au/Cu porphyry mineralization.
A program of grid based soil sampling is presently underway, and it
is planned to drill test the Elang target at the conclusion of
drilling at the Kuliuta gold prospect.
The New Hanover Project
New Hanover is an outstanding opportunity for the discovery of
Lihir-style gold mineralisation in a geological terrane that has
been bypassed by modern mineral exploration for the past 22 years.
The project comprises two 100% owned exploration licences (EL 1566
& ELA 1856) covering 591.6 km2 at the northwestern end of the
Lihir-Tabar alkaline volcanic belt, host to the giant Lihir and
Simberi gold deposits. Andesitic-dacitic volcanic rocks are
widespread on New Hanover. They were erupted from a coalesced
complex of Late Miocene-Early Pliocene stratovolcanoes that were
built upon older Late Eocene-Late Oligocene submarine andesitic and
basaltic rocks. Diorite, microdiorite and micromonzonite stocks
intrude the younger volcanic rocks. Of particular interest is the
presence of alkalic rocks, having relatively low silica content and
enriched in sodium and potassium, at the Kuliuta epithermal gold
prospect, indicating that New Hanover is geologically related to
the Plio-Pleistocene Lihir-Tabar chain of alkaline volcanic
islands.
Further details of the New Hanover project are available at
www.papuanpreciousmetals.com/project-newhanover.html.
The technical information in this news release has been prepared
in accordance with the Canadian regulatory requirements set out in
National Instrument 43-101 and reviewed on behalf of the Company by
Ian David Lindley, President & Chief Operating Officer of
Papuan Precious Metals Corp, a Qualified Person. Dr. Lindley has
First Class Honours and Ph.D. degrees in Geology, 34 years mining
industry experience, and is a member of the Australian Institute of
Geoscientists.
This press release contains "forward-looking information"
Forward-looking information is subject to known and unknown risks,
uncertainties and other factors that may cause PPM's actual
results, level of activity, performance or achievements to be
materially different from those expressed or implied by such
forward-looking information. Such factors include, but are not
limited to: uncertainties related exploration and development; the
ability to raise sufficient capital to fund exploration and
development; changes in economic conditions or financial markets;
increases in input costs; litigation, legislative, environmental
and other judicial, regulatory, political and competitive
developments; technological or operational difficulties or
inability to obtain permits encountered in connection with
exploration activities; and labour relations matters. This list is
not exhaustive of the factors that may affect our forward-looking
information. These and other factors should be considered carefully
and readers should not place undue reliance on such forward-looking
information. PPM disclaims any intention or obligation to update or
revise forward-looking information, whether as a result of new
information, future events or otherwise, except as required by
law.
ON BEHALF OF THE BOARD
David Lindley, COO and President
Contacts: Papuan Precious Metals Corporation Greg Downey
1.866.979.7022 info@ppmpng.com www.papuanpreciousmetals.com or
www.ppmpng.com
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