TIDMMML
RNS Number : 9732N
Medusa Mining Limited
12 September 2011
Medusa Mining Limited
(ASX & LSE: MML)
12 September 2011
BANANGHILIG DRILLING VERIFYING RESOURCE and EXTENDING
MINERALISATION
Medusa Mining Limited ("Medusa" or the "Company"), through its
Philippines operating company Philsaga Mining Corporation, advises
that the drilling at the Bananghilig Gold Deposit is verifying the
resource of 650,000 ounces and extending mineralisation laterally
and to depth.
The Bananghilig Deposit is within the regional scale Tambis
intrusive-breccia complex where the mineralisation is associated
with a combination of multiple diatreme breccias,
northeast-trending structures and various intrusive rocks.
Highlights include:
Grade (uncut)
Hole Number Width (metres) (g/t gold)
TDH 047 18.30 2.23
TDH 052 18.85 2.09
TDH 062 23.40 2.33
TDH 086 12.35 2.74
TDH 097 11.65 4.87
TDH 100 8.25 8.67
TDH 102 5.30 20.14
Geoff Davis, Chairman of Medusa commented:
"We are on our way! It is very pleasing to be able to report
that new drilling is verifying and extending the historical
drilling results on which the Bananghilig resource is based. The
geology is complex but now with 93 new holes already completed, a
good understanding of the geology and mineralisation controls is
taking shape. This mineralised system has the potential to grow
significantly beyond the three open zones already being defined and
totalling approximately three kilometres of mineralisation.
The diatreme breccia is open to the south below younger shallow
sediments, and we expect possible additions in this direction, as
well as along the extensive northeast-southwest structural
corridors.
Drilling will continue into 2012."
BACKGROUND
The Tambis Project, containing the Bananghilig Gold Deposit as
shown on Figure 1, is operated under a Mining Agreement with Philex
Gold Philippines Inc. over Mineral Production Sharing Agreement
("MPSA") 344-2010-XIII which covers 6,262 hectares.
The area has been known as an alluivial gold producing area
since Spanish times. The first modern exploration pre-Medusa group
was conducted in the 1970s followed by further work in the 1990s.
The Company commenced a concerted effort in July 2010 and drilling
prior to this is summarised in Table I.
Table I. Summary of the historical drilling statistics for
Tambis-Bananghilig Project area
Company Timeframe RC Drilling DD Total
Holes Metres Holes Metres Holes Metres
Sorex 1973-1977 33 3,633.36 33 3,633.36
Philex 1995-1997 227 12,628.70 79 12,172.85 306 24,801.55
Philsaga 2005-2007 31 7,753.50 31 7,753.50
TOTAL 227 12,628.70 143 23,702.71 370 36,188.41
Abbreviations:
Sorex: A. Soriano Corporation (on behalf of Atlas Consolidated
Mining and Development Corporation ("ACMDC")
Philex: Philex Gold Philippines Inc. ("Philex")
Philsaga: Philsaga Mining Corporation
In 2009, Cube Consulting Pty Ltd estimated Inferred Resources
for the deposit based on the historical drilling as shown in Table
II. The timing of a new resource estimate will depend on drilling
progress.
Table II. Bananghilig Deposit Resource estimate as at August
2009
Cut-off
(g/t gold) tonnes g/t gold ounces
0.50 20,000,000 1.1 730,000
0.60 15,000,000 1.3 650,000
0.70 12,000,000 1.5 580,000
0.80 10,000,000 1.7 530,000
0.90 8,000,000 1.9 480,000
1.00 7,000,000 2.1 440,000
Additional recent regional geological and mineralisation
information is contained in the announcement dated 10 May 2011.
AIM OF PROGRAMME
In July 2010, new regional and detailed mapping and drilling
programmes were commenced with the aim of validating the current
resource and extending it to provide a reserve of approximately
1,000,000 ounces. This reserve would form the basis for a
feasibility study which would target production of 200,000 ounces
of gold per year from a new milling facility.
REGIONAL GEOLOGICAL SETTING
The Tambis regional geology, termed the Tambis intrusive-breccia
complex, typifies a structurally complex intermediate-sulphidation,
epithermal gold, breccia-type system, including disseminated gold
overprinting the host Tertiary-age igneous package which had been
emplaced into an andesitic volcanic basement. The fertile igneous
suite comprises a multi-phase calc-alkaline, high level,
sub-volcanic intrusive package cut by extensive bodies of
phreatomagmatic diatremes and hydrothermal breccias.
Laboratory studies including fluid inclusions have indicated
that the Tambis area is only shallowly eroded with an estimated 500
to 950 metres of material stripped from the original surface.
The Tambis intrusive-breccia complex is overlain by younger
marine limestones and basal mudstones to the south and the east.
The extent of the complex below this younger cover is yet to be
determined.
Figure 1 (please see the link at the end of this announcement)
shows the location of the Tambis intrusive-breccia complex
BANANGHILIG DEPOSIT DESCRIPTION AND MINERALISATION
Introduction
Figure 2 shows that the Bananghilig Deposit currently consists
of three zones, each approximately 1 kilometre long and open in all
directions, locally termed the Sorex, Garden and Malinao zones.
These zones are broadly defined on the basis of the projection in
plan of >=0.5 g/t gold drill hole intersections. The bulk of the
current resources are in the Sorex and Garden zones.
Figure 3 shows the cross section through line 10710N. Assays
above 0.5 g/t gold are depicted in histograms.
In breccia hosted deposits the mineralisation is commonly not
uniformly disseminated or distributed due the presence of
fragments/clasts/blocks in finer matrix material, ie, the host rock
to the mineralisation is extremely inhomogeneous. Consequently the
location of the mineralisation within the breccias is influenced
not only by the structural emplacement of veins, breccias/fractures
and disseminations, but also by the relative distribution of the
fragments and matrix and the susceptibility of each to
mineralisation. This style of mineralisation should be considered
as a bulk mining proposition where mineralised domains are
established, and generally cannot be evaluated simply on the basis
of individual assay intervals.
Deposit Geology and Mineralisation
The Bananghilig Deposit (Fig. 2) is located partly within
diatreme breccias which measure at least 1,000 metres west to east
and still open to the south beneath the younger sediments, and also
around the diatreme margins and in the country rocks along
structural corridors.
The diatreme breccias contain unsorted fragments of the
andesitic basement as well as fragments of the later intrusive
rocks predating the diatreme events in a matrix of comminuted rock
flour and magmatic crystals. Fragment sizes range from
granule-sized to building-sized mega-blocks which have been torn
off the walls of the diatreme during the multi-episodal explosive
activity. The explosive activity also fractured the mega-blocks and
wall rocks, preparing them for subsequent mineralisation
deposition. The cross-section in Figure 3 shows several of the
mega-blocks which are the same composition as the wall rocks in
this area.
After the diatreme formation, several events of hydraulic
fracturing, hydrothermal and fault brecciation, rock alteration,
quartz veining and precious- and base-metal mineralisation
occurred. Based on mineral associations and fluid inclusion
results, the main gold deposition event appears to have occurred
following multiple hydrothermal fracturing along the margins of,
and within the diatreme complex. High gold concentrations appear to
be associated with elevated Ag and base metals.
The gold mineralisation style (+Ag +/-Zn +/-Cu +/-Pb) is
classified as an intermediate sulphidation epithermal system. In
and immediately adjacent to the diatreme, the gold mineralisation
generally occurs in vein-like zones, in fractures and/or breccia
in-fill in milled/fluidised muddy matrix breccia bodies and
coarsely brecciated/fractured andesitic-dacitic wallrock. It should
be noted that the vein zones shown on Figure 2 that are in the area
of the younger sediments are projected from below the limestone
contact.
Breccia veins in the deposit exhibit epithermal mineral growth
textures and in particular are related to retrograde boiling of the
mineralizing fluids. Major hydrothermal breccia veins are
sub-vertical to steeply dipping, averaging one metre thick, and
form anastomosing pinch-and-swell patterns up to several hundred
meters along strike. They are commonly offset in many places by
post mineralisation faults. Down dip continuity of breccia vein
mineralisation has been demonstrated to persist down to 500 meters
from surface. The breccia veins generally form a northeast-trending
sub-parallel array with minor north-south and east-west trends.
Widespread silica-illite-pyrite hydrothermal alteration affects
the volcanic wallrocks, the various breccia bodies and the
hypabyssal intrusives associated with them. The pervasive
near-surface argillic alteration haloes grade laterally and
vertically at depth into chloritic and propylitic alteration
assemblages.
Figure 2 (please see link at the end of this announcement) shows
the interpreted geological map showing drill hole locations and
section line 10710N.
Firgure 3 (please see link at the end of this announcement)
shows the cross-section 10710N through the Sorex and Garden
Zones.
DRILL RESULTS
Since 24 July 2010 to 31 August 2011, 32,311.05 metres of
diamond drilling in 93 holes have been completed. The drilling is
on-going with 7 rigs in the area.
Figure 2 shows the post July 2010 drill hole locations as blue
dots and drill hole traces for all the drill holes with assays
available (TDH 027 to TDH 102) at 31 August 2010. All pre-July 2010
drill holes are shown as black dots for collar positions.
First pass assaying for gold has been undertaken on all samples
submitted to the laboratory. Additional assaying is underway from
selected intervals for base metals, silver and other elements.
The results are summarised in Table II where significant
intercepts are defined on the following basis:
(i) lower cutoff grade of 0.5 g/t Au, and
(ii) >= 5 metres downhole intercept width at >= 0.5 g/t
Au, or
(iii) <= 5 metres downhole intercept width at >= 5
gram*metres, and
(iv) maximum of 3 metres of downhole internal dilution at
<=0.5 g/t Au.
Table II. Sorex and Garden zones surface drill hole results.
Grade
(uncut)
Hole Dip Azimuth From Width (g/t
number East North ([deg]) ([deg]) (metres) (metres) gold)
TDH
027 612978 945781 -50 130 175.10 5.00 1.12
248.45 2.00 2.86
287.65 2.00 10.12
302.00 7.00 1.16
TDH
028 612548 945822 -47 150 24.60 2.00 5.97
30.10 2.00 2.60
56,00 9.00 0.70
226.20 0.70 14.70
261.30 5.05 1.47
295.25 4.00 1.53
303.25 4.80 2.81
TDH
029 612774 945977 -47 130 58.90 3.50 1.49
109.50 7.30 1.97
TDH
031 612495 945757 -47 130 100.00 6.05 0.63
194.60 5.40 0.99
217.00 9.00 1.19
312.60 4.40 4.82
TDH
032 612846 946086 -47 130 40.70 2.40 19.70
TDH
034 612425 945658 -47 130 108.25 3.30 2.07
170.10 6.00 0.97
187.10 3.00 2.26
196.10 6.65 0.81
222.05 5.00 1.17
346.60 5.25 1.04
TDH
035 612639 945634 -47 130 58.70 2.70 2.69
141.75 1.20 36.05
196.70 4.50 1.13
242.30 5.15 0.58
TDH
036 612468 945649 -47 130 9.70 7.30 6.81
38.40 2.00 2.99
101.25 2.00 41.19
195.20 5.00 1.42
240.80 4.65 1.41
TDH
037 612693 945708 -47 130 110.50 2.00 4.50
159.50 23.00 0.66
243.05 6.00 0.72
309.65 6.00 1.93
Grade
(uncut)
Hole Dip Azimuth From Width (g/t
number East North ([deg]) ([deg]) (metres) (metres) gold)
TDH 038 612381 945693 -47 130 90.20 11.25 1.30
TDH 039 612595 945680 -47 130 104.05 2.00 4.91
122.80 18.50 1.67
158.30 7.00 0.75
TDH 040 612465 945782 -47 130 47.90 3.00 1.93
195.70 1.20 4.75
222.50 7.00 6.10
TDH 041 612720 945170 -47 310 8.90 15.20 0.95
113.50 20.00 0.80
163.70 6.35 0.98
TDH 042 612595 945680 -47 130 25.75 1.00 11.33
88.65 4.75 1.16
108.10 5.85 0.92
126.35 14.00 0.79
182.30 6.55 0.93
226.00 3.40 2.02
235.30 1.00 8.48
209.25 8.50 1.04
320.05 5.00 1.82
TDH 043 612757 945123 -47 310 10.50 2.35 2.24
44.80 6.90 0.75
86.60 15.65 1.24
227.65 3.00 1.79
240.25 6.00 1.14
309.05 8.55 0.80
TDH 045 612696 945811 -47 130 125.05 6.00 0.67
271.20 5.70 1.18
359.15 8.85 1.68
398.85 21.40 1.04
483.90 3.10 3.22
504.50 8.10 2.80
TDH 046 612755 945121 -47 130 68.15 8.45 0.95
79.60 7.00 1.19
TDH 047 612720 945169 -47 130 85.30 0.50 54.39
163.90 18.30 2.23
TDH 048 612902 946194 -47 130 138.50 1.00 32.20
TDH 049 51.05 3.65 7.12
58.70 5.60 0.78
TDH 050 612718 945171 -60 130 86.85 3.20 1.49
100.85 9.50 0.63
TDH 051 612757 945123. -60 130 84.55 13.05 2.27
106.10 5.90 2.46
116.00 8.00 0.87
132.00 36.70 1.07
196.35 5.50 1.00
TDH 052 612625 945044 -47 130 62.40 18.85 2.09
126.30 1.00 5.96
334.30 4.00 3.98
369.40 1.00 7.73
TDH 053 612739 945767 -47 130 288.25 10.00 0.77
TDH 054 612883 945232 -47 130 65.20 13.95 0.97
126.45 8.55 2.59
258.10 10.15 2.34
275.55 9.55 0.98
TDH 056 612624 945044 -47 310 0.65 6.50 0.81
66.20 6.00 0.77
TDH 058 613081 945395 -47 130 23.40 6.00 1.04
34.40 12.75 0.76
198.10 1.35 20.97
TDH 059 612465 944990 -60 130 54.35 7.80 1.17
112.85 6.00 1.33
122.05 9.45 1.12
TDH 060 612799 945340 -47 130 142.55 10.95 1.49
221.10 1.50 12.59
233.60 1.05 10.15
254.55 4.15 9.82
262.35 4.80 1.15
TDH 061 612557 945147 -47 130 17.60 4.30 1.89
TDH 062 612493 945421 -60 130 31.20 10.70 0.72
51.50 11.60 1.26
66.40 23.40 2.33
100.65 2.60 3.49
112.20 8.20 0.80
156.00 7.75 1.82
178.75 8.00 0.76
191.00 3.00 14.38
204.10 3.00 3.99
TDH 063 612849 945301 -47 130 187.50 1.00 6.21
212.90 4.60 1.22
246.15 4.65 1.11
TDH 064 612397 945291 -60 130 58.75 1.00 5.65
125.45 9.40 1.28
TDH 065 612916 945151 -60 130 115.80 7.95 1.04
195.45 6.60 1.30
TDH 066 612799 945340 -60 310 188.00 2.05 3.18
219.60 3.40 2.35
TDH 067 612721 945476 -47 130 43.30 5.40 10.93
TDH 068 612798 945184 -60 130 13.55 2.35 5.80
TDH 069 612612 945326 -47 130 14.45 3.00 2.00
23.35 3.00 3.01
101.45 6.55 1.83
253.10 3.70 3.04
TDH 070 612869 945118 -60 130 77.75 20.55 0.91
102.70 10.00 3.12
187.45 7.15 0.86
400.45 5.00 4.13
TDH 071 612805 945267 -47 130 52.70 7.60 0.86
234.90 2.70 5.98
253.65 2.90 2.47
293.80 1.90 4.70
TDH 072 612673. 945130 -60 130 31.10 10.30 0.83
89.70 11.70 0.90
TDH 073 612673 945205 -60 130 221.70 10.90 1.12
TDH 074 612727 945077 -60 130 110.35 5.20 0.82
125.85 8.95 1.49
TDH 076 612801 945405 -60 130 94.20 7.75 1.12
128.35 5.60 1.54
TDH 077 612965 945170 -60 130 81.20 1.25 8.08
142.70 6.30 0.71
196.00 4.85 2.09
TDH 078 612756 945211 -60 130 76.25 1.00 45.00
97.20 25.20 0.78
TDH 080 612863 945370 -60 130 118.30 2.85 45.12
TDH 081 612537 945346 -60 130 41.90 1.55 6.15
47.95 6.65 0.81
196.30 3.15 1.66
TDH 082 612788 944959 -60 130 298.35 9.25 2.43
TDH 083 612910 945425 -60 130 196.60 1.00 34.00
219.55 6.20 2.97
TDH 084 612763 945433 -60 130 85.25 1.80 6.02
102.45 5.15 0.57
166.75 24.80 0.82
TDH
085B 612570 945371 -70 130 12.90 7.10 1.90
48.00 20.35 1.61
108.65 20.35 1.63
147.05 7.00 2.65
TDH 086 613012 945384 -60 130 5.35 20.55 1.73
54.65 1.00 5.63
152.30 12.85 0.68
185.45 12.35 2.74
TDH 087 612560 945067 -60 130 64.20 3.60 1.61
90.15 11.25 1.11
104.40 9.20 1.81
132.60 13.00 0.60
185.05 7.00 6.19
202.80 8.50 0.99
267.85 7.00 0.65
TDH
088B 612664 944986 -50 130 7.25 8.95 3.48
26.00 9.20 0.82
114.55 6.35 0.90
129.90 6.25 2.13
TDH 089 612602 945191 -60 130 57.85 2.30 3.62
170.80 6.00 0.73
TDH 090 612898 945096 -60 130 107.60 12.45 1.13
126.05 14.25 1.39
233.80 6.00 0.59
TDH 092 612436 945484 -60 130 118.35 13.05 1.33
154.90 1.70 4.32
189.85 3.25 3.59
264.60 4.90 1.03
TDH 093 612722 945475 -70 310 195.30 7.80 2.50
273.05 1.00 10.72
TDH 094 612631 944946 -60 130 7.80 10.60 1.18
56.95 8.00 0.71
71.40 5.00 0.57
TDH 095 613043 945413 -60 130 8.70 12.05 0.79
198.95 6.00 0.64
285.00 2.00 5.16
323.90 3.00 2.15
359.15 3.80 1.33
405.20 18.25 1.10
TDH 096 612452 945412 -70 130 12.15 6.05 1.12
33.30 8.05 0.81
44.35 4.00 2.27
76.40 1.00 6.16
277.60 8.00 0.60
TDH 097 612429 945257 -60 130 43.95 11.65 4.87
162.05 6.20 1.58
TDH 098 612583 945502 -60 130 24.30 9.80 0.88
58.60 3.70 1.65
82.80 4.15 1.30
90.80 3.65 5.03
258.60 8.00 0.62
TDH 099 612863 945209 -60 130 176.95 2.30 8.66
188.15 7.20 2.93
213.55 4.30 9.26
TDH 100 612831 945073 -60 130 112.75 2.85 3.88
378.95 8.25 8.67
413.30 2.00 2.55
650.95 12.85 1.83
TDH 102 612770 945368 -47 130 109.70 5.40 4.17
129.50 5.85 0.87
137.35 5.30 20.14
173.40 5.55 3.72
Notes:
(i) Intersection widths are downhole drill widths not true
widths;
(ii) Assays denoted by (*) are by Philsaga Mining Corporation's
laboratory, all other assays are by McPhar Geoservices Inc. in
Manila;
(iii) Check surveying of collar positons in progress;
(iv) Grid coordinates based on the Philippine Reference System
92.
DISCUSSION OF RESULTS AND STATISTICAL COMPARISONS
Statistical comparisons have been undertaken between the two
historical drilling assay data sets and the new drilling assay data
set. The drilling since July 2010 supports the grade tenor shown by
the historical drilling, particularly the drilling by Philex. The
Sorex drilling was more concentrated on a higher grade zone in the
northwest part of the Sorex zone which may have skewed the Sorex
data set. However when the higher grade subsets and the lower grade
subsets are compared, the subsets are statistically comparable.
Drilling was undertaken to twin some of the historical
drillholes of Sorex, Philex and Philsaga. Drill hole TDH 062 was
the first drill hole to be completed in the Sorex area. Results
from this hole correlate well with nearby drilling considering the
nature of the mineralisation.
The recent drilling has extended the limits of the known
mineralisation to the northeast and southwest along the strike of
each of the Malinao, Sorex and Garden zones, and southeast beneath
the younger sedimentary sequence, and at depth.
Essentially the mineralisaton is open in all directions with the
potential for the discovery of additional resources.
DRILL HOLE SAMPLING AND ASSAYING PROCEDURES
Drilling Procedures
Drilling, sampling and analytical methodologies are of
internationally acceptable standards. Drilling and analyses are
carried out by independent contractors, SBF Philippines Drilling
Resources Corp. (SBF), and Intertek Testing Services Philippines,
Inc. (Intertek) respectively.
Drilling is carried out by SBF using wireline diamond coring
techniques, with the core being predominantly HQ triple-tube (HQ3)
diameter (OD 61mm). The holes are initially collared using PQ
drillbits (OD 123mm) to recover PQ3 core (OD 83mm) until the
drillbit encounters competent ground, then the coring bit is
reduced to HQ3 for the remainder of the drill hole. If difficult
conditions are encountered, then the drill bit is changed to NQ3
(core OD 45mm) and the hole continued until the planned depth or
bad ground conditions prevent further drilling, whichever occurs
first. Core recovery is generally better than 95% and is considered
to be good.
Drill Core Sampling
Drill core is recovered from the inner tube and handled
carefully to preserve the integrity of the drill core. Structural
measurements are taken: Rock Quality Determinations (RQD,) and
Fracture Densities. The core is then placed in plastic core trays,
aligned, photographed and marked up for sampling.
The drill core is then cut in half by diamond core saw and
sampled at one (1) metre intervals or at lithological boundaries.
The samples are placed in individually labelled plastic sample
bags, a sample number ticket included, and then sealed for despatch
to Intertek's Sample Preparation laboratory in Surigao City. The
integrity of the core samples are supervised at all times by the
geologist until despatch to the laboratory where they are
accompanied by company personnel until receipt by Intertek.
One Certified Reference Material (CRM), one Blank and if
possible, one Duplicate is included within each successive group of
twenty samples that are submitted to the laboratory. QA/QC
monitoring of the drilling program and the results is ongoing.
Analytical Procedure
Sample preparation is undertaken by Intertek at their Surigao
City laboratory, where each sample is registered, dried at 105 C
for 6 to 8 hours and crushed to 95% passing 2 mm by jaw crusher,
before a 1kg split is taken for fine pulverising, using a riffle
splitter or rotary sample divider. Pulverised sample is nominally
pulverised to 95% passing 75<MU>m (200 mesh).
Quality control procedures include a 1 in 15 resplit after
crushing for partial preparation and after pulverising for total
preparation. These resplits are also analysed and included in the
analysis report. Sizing tests are carried out on 1 in 20 assay
pulps at 75<MU>m (200 mesh) to monitor the pulverising stage.
Four 250 gram splits are obtained, one for sample analyses and the
remaining three for storage for future reference.
Standard laboratory procedure is to clean the crusher and
pulveriser after each sample treatment with barren material and/or
bowl wash, to minimise carry-over contamination.
Pulverised samples are analysed by classical fire assay
techniques on a 50 gram charge with Atomic Absorption Spectrometer
(AAS) finish. All assays over 5 g/t gold and other selected samples
are re-assayed using gravimetric fire assay techniques on a 50 gram
sample.
[INSERT LINK]
For further information please contact:
Australia
Medusa Mining Limited +61 8 9367 0601
Peter Hepburn-Brown,
Managing Director
Geoff Davis, Chairman
United Kingdom
Fairfax I.S. PLC +44 (0)20 7598 5368
Nominated Adviser
and Broker
Ewan Leggat/Laura
Littley
Information in this report relating to Exploration Results has
been reviewed and is based on information compiled by Mr Geoff
Davis, who is a member of The Australian Institute of
Geoscientists. Mr Davis is the Chairman of Medusa Mining Limited
and has sufficient experience which is relevant to the style of
mineralisation and type of deposits under consideration and to the
activity which he is undertaking to qualify as a "Competent Person"
as defined in the 2004 Edition of the "Australasian Code for
Reporting of Exploration Results, Mineral Resources and Ore
Reserves" and is a "Qualified Person". Mr Davis consents to the
inclusion in the report of the matters based on his information in
the form and context in which it appears.
Information in this report relating to Mineral Resources has
been estimated and compiled by Mark Zammit of Cube Consulting Pty
Ltd of Perth, Western Australia. Mr Zammit is a member of The
Australasian Institute of Mining & Metallurgy and has
sufficient experience that is relevant to the style of
mineralisation and type of deposit under consideration and to the
activity which he is undertaking to qualify as a Competent Person
as defined in the 2004 Edition of the "Australasian Code for
Reporting of Exploration Results, Mineral Resources and Ore
Reserves". Mr Zammit consents to the inclusion in the report of the
matters based on his information in the form and context in which
it appears.
DISCLAIMER
This announcement may contain certain forward-looking
statements. The words 'anticipate', 'believe', 'expect', 'project',
'forecast', 'estimate', 'likely', 'intend', 'should', 'could',
'may', 'target', 'plan' and other similar expressions are intended
to identify forward-looking statements. Indications of, and
guidance on, future earnings and financial position and performance
are also forward-looking statements.
Such forward-looking statements are not guarantees of future
performance and involve known and unknown risks, uncertainties and
other factors, many of which are beyond the control of Medusa, and
its officers, employees, agents and associates, that may cause
actual results to differ materially from those expressed or implied
in such statements.
Actual results, performance or outcomes may differ materially
from any projections and forward-looking statements and the
assumptions on which those assumptions are based.
You should not place undue reliance on forward-looking
statements and neither Medusa nor any of its directors, employees,
servants or agents assume any obligation to update such
information.
This information is provided by RNS
The company news service from the London Stock Exchange
END
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Medusa (LSE:MML)
Historical Stock Chart
From Jun 2024 to Jul 2024
Medusa (LSE:MML)
Historical Stock Chart
From Jul 2023 to Jul 2024