Quantcast

Radius Provides Update on Eastern Guatemala Gold/Silver District

May 5, 2011

VANCOUVER, May 5 /PRNewswire/ – Radius Gold Inc. (TSX-V: RDU) is pleased to
provide a comprehensive update on its recent exploration activities in
the highly prospective low-sulphidation epithermal gold-silver district
in eastern Guatemala. Radius holds over 1,500 sq. km. of granted
concessions and concession applications in the region covering a
virtually unexplored Tertiary volcanic belt that has recently been
shown to host world class intermediate and low sulphidation silver/gold
deposits.

Recent highlights of Radius’ work include:

        --  Delineation of an impressive zone of high-level chalcedonic
            silica currently traced for over 400m along strike and over
            100m wide locally within the Zapote trend of the HB property.
            Initial sampling of outcrop at Zapote has returned gold values
            from a low of 0.50 to a high of over 6.0 g/t Au. Trenching and
            extensive outcrop sampling are presently underway.
        --  Identification of a high grade zone on the north side of the
            Holly ridge. Previous prospecting and sampling in this area
            discovered quartz boulders believed to be float, grading from
            just under 1 g/t Au up to 112 g/t Au and over 5,600 g/t Ag.
            Trenching in the area has revealed texturally-similar quartz
            veins in situ in the schists directly below the boulders. This
            is a significant find as little work has previously been done
            on the north side of the Jocotan fault, despite the presence of
            large, coherent, untested gold in soil anomalies there.
        --  Completion of 14 diamond drill holes into the Pyramid Hill and
            M28 zones. Drill results are disappointing (see below).
            However, a structural study of drill core and outcrop by SRK
            confirms a strong northwest trending gold bearing fault zone
            with a strike of over 3km that has been tested only at very
            high levels. The study results indicate that Radius' work has
            been focused above the "productive zone" of the epithermal
            system. Additional drilling is being planned to target
            substantially deeper levels than any previous work at HB.

Zapote Zone

The Zapote zone is southwest of, and probably parallel to the M28 /
Pyramid Hill zones. At surface the zone is an impressive, steeply
west-dipping vein exposed with a true thickness of between 5 to 10m,
although the orientation is still uncertain. The distribution of float,
subcrop, and small veinlet orientation suggests the presence of another
mineralized vein with a different orientation to the one described
above, although more work is necessary to confirm that.

Trenching is underway, and all samples collected to date are highly
anomalous in Au (i.e. in the ppm range). The first 23 samples collected returned an average
grade of 2.01 g/t Au, ranging from 0.50 to 6.0 g/t Au. Systematic
sampling and trenching should help define the true width and nature of
the vein(s).

Zapote appears to be high in a hydrothermal system: massive chalcedony
dominates in outcrop. Radius’ geologists believe that there is
potential at depth for better grades, which could present a very
attractive drill target if the vein stays as thick as it appears to be
at surface.

The Pino Zone

A data review by Radius highlighted 17 historic grab samples of
electrum-bearing epithermal vein quartz collected from the Pino zone, a
low sulphidation epithermal quartz vein hosted by schists on the
northwestern side of the HB project. Gold assay results from the 17
samples ranged from just under 1 g/t Au to 112 g/t Au, with an average
of 19.8 g/t Au. Silver values range from trace to 7,091.8 g/t Ag.

Radius’ historic exploration in the area focused on the younger volcanic
rocks to the south of the major Jocotan fault. The grab samples
reported below were collected from the schists on the northern side of
the fault, and were previously interpreted as transported float rocks
not in situ. Radius’ geologists have trenched below the float samples and
encountered similar material hosted by the schists, suggesting that the
high grade float reflects the presence of veins in the schists and is
not transported material. Assay results are expected in the next 2
weeks from the trench samples and a table of the most significant
historic grab sample results is given below:


    Sample # Au (g/t) fire assay Ag (g/t)

      18258           112.41     5,600.0

      18256            79.28     7,091.8

      18257            33.75     1,030.0

      12296            27.98     1,423.4

      18253            19.96       237.3

      11093            14.38       880.7

      18255            11.18       401.1

      16067             7.67       258.6

      18286             6.51       201.3

      18254             4.46        97.0

      18264             3.64        14.7

      18289             3.15        35.9

      16083             3.90        10.4

      11092             3.49        18.8

      17018             1.78         Tr

      17038             1.30         Tr

      17023             0.96        9.4

M28 / Pyramid Hill Drilling

Forty-nine holes have been drilled at Banderas since 2002 including 6 RC
holes. Most drilling has targeted the M28 and Pyramid Hill zones, part
of a 3 kilometre long, northwest-southeast-trending structural corridor
that hosts zones of gold/silver-bearing quartz veins, vein breccias and
quartz vein stockwork zones. A comprehensive in-house review of Radius’
full data set on the HB project is currently underway, and SRK
Consulting (Canada) Inc. has been commissioned to complete a structural
geological study of the project.

The initial findings of both studies, combined with the findings of a
TerraSpec study on the alteration minerals present at surface and in
core samples at HB, suggest that Radius’ drilling is still testing too
shallow in the epithermal system and has not reached what would be
termed the “productive horizon” where economic gold and silver grades
would be expected to occur over mineable widths. The work is indicating
that drilling needs to target between 300-700m vertically below the
paleo water table. Interestingly, RC drill hole BRC04-024 cut an
argentite-bearing quartz vein over 1.5m core length which graded 69.97
g/t Au + 516 g/t Ag, and is both the highest grade and deepest drill
intersection on the Banderas property.

Consequently, Radius has stopped drilling at HB until the full data
review is complete. Management currently anticipates that the project
review will result in a recommendation for a major drill program to
commence later in 2011 or early 2012.


     Hole*  From (m) To (m) Width (m) Au g/t Ag g/t

    10-008    73.43  77.03     3.60    0.84   12.0

    10-009    NSV**     -         -      -      -

    10-010     NSV      -         -      -      -

    10-010A    NSV      -         -      -      -

    10-011     NSV      -         -      -      -

    10-012   192.32  193.60    1.28    0.32   36.6

    10-013    61.53  62.53     1.00   38.35  159.9

    10-013    68.75  75.30     6.55    0.56  239.8

     incl.    68.75  69.75     1.00    1.34   95.4

    10-014    25.08  27.43     2.35    1.46   14.0

    10-014    74.00  75.10     1.10    0.82   48.1

    10-014   136.64  137.64    1.00    12.3   37.3

    10-014   179.65  181.00    1.35    18.1   20.9

*All holes carry the prefix BDD **NSV=No Significant Values (<250 ppb
Au, <10 ppm Ag)

Background

The Holly and Banderas projects (HB) were discovered by Radius during a
regional stream sediment sampling program in Eastern Guatemala
conducted in 2001/2. The projects are close together and are now being
considered as a single exploration project, the HB project.

Sampling Methodology, Quality Control, and Assurance  

The 2010/2011 diamond drill program used man-portable drills sampling
NTW and HTW (5.6 cm/ 2.2″ and 7.11 cm/ 2.8″) core size. Core is cut and
one-half sent to the lab for analysis, the other retained on site.
Surface samples are from float, outcrop, and hand-dug trenches. 

The core and surface samples are sent to the Inspectorate Guatemala
sample preparation facility in Guatemala City for sample preparation,
and pulps forwarded to the Inspectorate American Corporation laboratory
facility in Sparks, Nevada, for analysis. Approximately 12% of the
samples submitted consist of commercial standards, blanks, and
duplicate samples. These are included with each batch sent to the
analytical laboratory. Gold amounts for each sample are determined by
fire assay, digested in aqua regia solution and analyzed by atomic
absorption finish. Samples with over 1 g/t Au are re-analysed by
gravimetric finish. Ag is analysed by aqua regia digestion followed by
atomic absorption finish with overlimits analysed by fire assay with
gravimetric finish. A 30 element suite is analysed by ICP. 

Assay results reported here for surface grab samples from the Pino zone
should be considered historic, as detailed QA/QC protocols are not
available for the time period (2002-2003). Samples were analysed by
Inspectorate, in Sparks, Nevada, by fire assay with atomic absorption
or gravimetric finish for Au, and aqua regia digestion with ICP finish
for a 30 element suite. 

Drilling Sampling Protocol, Chain of custody, and Data Verification 

All sampling is conducted under the supervision of the Company’s on-site
project geologist and the chain of custody from the drill to the
logging facility is continually monitored. Samples are transported to
the Inspectorate facility in Guatemala City directly by Company
personnel. Data verification of the analytical results includes
analysis of the duplicates, standards and blanks to ensure that they
pass industry best practise guidelines for acceptability. All assays
are reported as drilled intervals.

Qualified person

Roger Hulstein, BSc, is a member of the Association of Professional
Engineers and Geoscientists of British Columbia and is the Company’s
Qualified Person as defined by National Instrument 43-101. Mr. Hulstein
is responsible for the accuracy of the technical information in this
news release.

About Radius

Radius has been exploring for gold in Latin America for nearly a decade,
and has assembled interests in a portfolio of promising gold projects
throughout the region, including carried stakes in two small-scale
developing gold projects in Guatemala and Nicaragua.  Radius also has a
number of 100% owned exploration plays, including the HB property in
Guatemala and several properties in the Rackla Belt and Sixty Mile
placer gold district in the Yukon.

ON BEHALF OF THE BOARD
     “Simon Ridgway”
Simon Ridgway, President & CEO

Investor relations:  Ralph Rushton / Erin Ostrom
Symbol: TSXV-RDU; OTCBB-RDUFF
Shares Issued: 79.9-million

Forward-Looking Statement
Some of the statements in this news release contain forward-looking
information that involves inherent risk and uncertainty affecting the
business of Radius Gold Inc.  Actual results may differ materially from
those currently anticipated in such statement.

Neither the TSX Venture Exchange nor the Investment Industry Regulatory
Organization of Canada accepts responsibility for the adequacy or
accuracy of this release.

SOURCE Radius Gold Inc.


Source: newswire



comments powered by Disqus