Medusa Mining Limited: Co-O Mine Geology and Mineralisation Update
(firmenpresse) - TORONTO, ONTARIO -- (Marketwire) -- 08/14/12 -- Medusa Mining Limited ("Medusa" or the "Company") (ASX: MML)(LSE: MML), through its Philippines operating company Philsaga Mining Corporation, advises that
3. Major advances have been made during the year in understanding the Co-O Mine geology as summarised below:
Peter Hepburn-Brown, Managing Director commented:
"As we continue to extend the size of the area of mineralisation, our confidence in the validity of the Conceptual Exploration Target size is enhanced. This year has again justified that level of confidence.
We have made major advances in the understanding of the Co-O Mine geology and potential during the year. This has been highlighted by the identification of extensive porphyry-related copper-gold mineralisation with the potential that it is connected to a major primary porphyry copper-gold source in the immediate vicinity.
We are currently reviewing and re-interpreting significant zones of multiple epithermal veining and stockworks which will be investigated for bulk mining techniques.
It is still very apparent that the Co-O vein system is open in all directions providing potential for resource enhancements for many years."
(ii) The potential target size and grade is conceptual in nature, and there has been insufficient exploration to define a mineral resource, and it is uncertain if further exploration will result in the target being defined as a mineral resource.
Co-O MINE CONCEPTUAL TARGET (ii)
Drilling since the estimate of the Conceptual Exploration Target announced on 18 January 2010 has continued to expand the vein system, as supported not only by the 2012 global resource estimate of 2,019,000 ounces, but also by the 979 drill hole intersections greater than 2g/t gold over greater than 0.2 metres which are not yet included in the resource model.
The range for the Conceptual Exploration Target remains well supported at 3,000,000 ounces in 9,800,000 tonnes to 7,000,000 ounces in 23,500,000 tonnes using a grade range of 9 to 11 g/t gold with a preferred average grade of 10 g/t gold as shown in Table III.
The combination of past production of approximately 510,000 ounces and the current global resource of 2,019,000 ounces indicates the deposit size is approaching the lower end of the Conceptual Exploration Target size range.
The additional support for this target is listed below:
To view "Figure 1. Composite longitudinal projection of the Co-O Mine showing the diatreme and all drill hole intersections below Level 6," please visit the following link: .
To view "Figure 2. Composite longitudinal projection of the Co-O Mine showing the diatreme and the 979 drill holes not yet included in the resource model," please visit the following link: .
Co-O MINE LOCAL GEOLOGY
The Co-O Mine area is underlain by a probable Eocene (56 to 34 million years) to Oligocene (34 to 23 million years) age, gently north-dipping sequence of basaltic andesitic to andesitic volcanic flows and minor volcaniclastics (Fig. 3).
To view "Figure 3. Co-O Mine area interpreted geological map showing section lines A-A' and B-B'," please visit the following link: .
This sequence is intruded by Oligocene andesitic to dioritic stocks and dikes dated at 32 million years old and cut by north-trending steep faults with the Oriental Fault identified as the most significant fault to date (Sonntag & Hagemann, 2010).
There are three large outcropping intrusives, namely the Nangka, Road 17 and Pinayungan Intrusives, located east and southwest of the Co-O vein system, and several smaller ones in the vicinity. The Nangka and Pinayungan Stocks are in place while the rest are "floating" in the Co-O Diatreme including the large Road 17 Mega Block as explained below. At depth, Nangka Stock enlarges beneath the Co-O Diatreme to become a 400 metres east-west by greater than 800 metres north-south body.
Porphyry-related copper-gold mineralization is hosted only in the Nangka Stock and the surrounding volcanics (Figs 4 to 6).
After a period of substantial uplift and erosion, a diatreme/maar complex explosively intruded all the above rock types (Figs. 3 to 6). Its presence explains the general absence of near surface epithermal veins east of the Oriental Fault instead of invoking a large down thrown movement of the zone as the veins are masked by the flare of the diatreme.
Note: diatremes are generally caused by the explosive release of gases and fluids from the catastrophic mixture of ground water from the surface and magma at depth. These gases and fluids force their way to the surface, causing pipe-like columns of broken or brecciated rock that flare outwards near surface producing funnel shaped features that are often concave on the surface after the explosive activity has ceased. The clouds of rock fragments and dust that are released settle around the annulus of the diatreme and also on top of the diatreme. If the diatreme surface remains concave or a natural depression, younger sediments will commonly accumulate in the depression, frequently under a lake that forms in the depression.
To view "Figure 4. North-south cross section of the interpreted geology along section line A-A looking west," please visit the following link: .
To view "Figure 5. East-west longitudinal projection of the interpreted geology along section line B-B' looking north," please visit the following link: .
The Co-O Diatreme is upward flaring in all directions towards the surface, measuring about 1.5 kilometres in diameter, and narrows down at depth like a funnel of unknown dimensions. Its root is probably located at the southern part of the Road 17 Intrusive. It is inferred that the diatreme may easily reach 1 kilometre or more in depth as indicated by its surface dimension wherein the vertical extent is more than its lateral extent. The maar volcanics, which are the extrusive equivalent of the diatreme and deposited by the explosive activity of the diatreme, are still largely intact in the eastern and partly in the northern fringe of the diatreme and some isolated preserved outcrops to the west side of the Oriental Fault. The maar rocks consist of andesitic crystal lithic tuffs, with some dacitic facies, sometimes exhibiting crude to laminated subhorizontal bedding, minor intercalations of tuff breccias, accretionary lapilli tuffs and thinly bedded carbonaceous tuffaceous mudstones (Photos 1 and 2). The presence of accretionary lapilli tuff would indicate base surge deposits which were emplaced by violent subhorizontal blasts emanating from the diatreme's throat.
To view "Photo 1. Contact of the upper andesite porphyry to diorite megablock with the underlying diatreme (Hole EXP093: 101 to 110.55 metres)," please visit the following link: .
Mega Blocks of the maar tuff and intrusive are floating in the diatreme representing fallen blocks and roof pendants in the upper part of the diatreme. The largest mega-block is the Road 17 Mega Block, about 400 metres wide by 800 metres long, located at the eastern portion of the diatreme and which is exposed on the surface (Figs 3 to 5 and Photo 1).
After the emplacement of the diatreme/maar complex, mineralised hydrothermal breccias followed by epithermal gold veins were formed, overprinting the older porphyry-related copper-gold mineralisation. The veins generally strike west-northwest to due west and dip 55 to 75 degrees to the north for all veins except the Central Vein which is vertically dipping.
Post-mineral re-activation of pre-existing north-trending faults, represented by the Oriental Fault and other sub-parallel faults, cut the epithermal veins, showing dextral (right lateral strike-slip) movement with a diagonal component (Standing & Noble, 2011). This faulting displaces the veins laterally to the south and downward by a few metres to several tens of metres.
After another episode of uplift and erosion, a thin veneer of polymictic conglomerate to a maximum thickness of about 30 metres, was deposited on top of the diatreme/maar complex (Fig. 3). The conglomerate consists of rounded to subangular clasts of all the pre-existing rocks including rare feldspar porphyry intrusive (which is common in the Tambis area), epithermal vein material, and petrified and young carbonised wood (Photo 2). This conglomerate contains alluvial gold.
To view "Photo 2. Polymictic conglomerate with carbonised wood and quartz vein clasts," please visit the following link: .
MINERALISATION
There are two mineralisation styles in the Co-O Mine area, namely the:
Since the epithermal gold veins are usually emplaced within about 1 kilometre from the paleo-surface while a porphyry copper system is emplaced at least 2 kilometres from the paleo-surface, there has been substantial uplift and passage of time between the two mineralisation events since the former overprinted the latter. Also, very little erosion of the epithermal veins has taken place since the older near-surface maar facies is still essentially intact. This is corroborated by the recent fluid inclusion study of Hagemann & Grignola (2012) which concluded that the paleo-depth of epithermal vein formation is about 61 to 295 metres.
Porphyry-related Copper-Gold Mineralisation
The porphyry-related copper-gold mineralisation is generally weak and is hosted in the Nangka Intrusive and the surrounding volcanics (Fig. 4). The mineralisation is not classical porphyry copper-gold since the alteration is chloritic to propylitic instead of the conventional potassic, sericitic and/or sericite-chlorite, and due to the local presence of lead-zinc sulphides together with chalcopyrite. Also the Nangka Intrusive is still considered a pre-mineral host rock and not the causative intrusive, i.e. the intrusive that brought about the mineralisation. This is evidenced by the fact that mineralisation is irregular in distribution within the stock, and consequently is currently termed "porphyry-related" copper-gold mineralisation.
The mineralisation occurs in four irregularly shaped discontinuous zones along a northerly trending corridor about 650 metres east-west by 850 metres north-south. The northern and southern mineralised zones are more developed than the centrally located ones. Also, the mineralised zones are positioned deeper towards the south. Figure 4 shows that the northern mineralised zone lies between the surface and mine Level 7, while the southern zone is generally at mine Level 4 to below Level 16, and that the mineralisation is confined mainly at the northern and southern margins of the stock (Fig. 4). The northern mineralised zone is 250 to 400 metres wide by 400 metres vertically while the southern zone is 150 to 300 metres wide by greater than 600 metres vertically. Vertical hole EXP127 on Figure 4 shows that the mineralisation is likely still open at greater than 1 kilometre below the surface as indicated in Table II.
Table II. Examples of porphyry-related copper-gold mineralisation intersections using 1g/t gold upper cut
The copper-gold mineralisation is characterised by sheeted to multi-directional less than 1 to 2 mm grey quartz-sulphide veinlets and rare sulphide fracture fills and disseminations. Veinlet density is about 2 to greater than 10 per metre. The sulphides consist of less than 1 to 3 % pyrite, less than 0.1 to 0.5 % chalcopyrite, and sporadic occurrence of sphalerite and galena. These veinlets are overprinted by epithermal veins in some areas as shown in Photo 3.
To view "Photo 3. Chloritic altered andesite porphyry intrusive with porphyry-related 2-3mm wide greyish quartz-sulphide veinlets (0.14 to 0.18% Cu & 0.14 to 0.23 g/t Au) overprinted by a 200 mm wide milky epithermal quartz vein (98.76 g/t Au) and other narrower ones. (Hole EXP089: 377.75 to 382.35 metres)," please visit the following link: .
The porphyry-related copper-gold mineralization is generally weak. Values range from 0.11 to a maximum of 0.31 % Cu and 0.11 to 0.24 g/t Au with a Cu:Au ratio of about 1:1 to 1:2.
It is the presence of epithermal gold veins/stockworks that increases the gold grade of the overprinted porphyry-related copper-gold mineralisation. Thirty eight EXP holes containing wide zones of both porphyry-related copper-gold and epithermal gold veins have been identified to date, some of which are shown in Table III. Other potential wide multiple vein zones outside the copper zone have also been identified, These zones will be considered for underground bulk mining as additional data becomes available and interpretation work progresses.
Table III. Examples of EXP holes with wide mineralisation zones using a 2 g/t Au intersection boundary cut-off
Epithermal Gold Mineralisation
The intermediate sulphidation epithermal gold mineralisation has overprinted the porphyry-related copper-gold mineralisation.
Initiation of the epithermal system is represented by structurally controlled, discontinuous, and commonly narrow less than 1 to 5 metre wide hydrothermal breccias which are sometimes mineralised but generally less than 1 g/t gold. A large barren hydrothermal breccia body, 75 metres by 270 metres, has been recognised at the south-western portion of the area (Fig. 3).
The hydrothermal breccias were followed by the formation of the main stage well-mineralised epithermal quartz veins which occasionally penetrated the edges of the diatreme/maar complex and sometimes cut the hydrothermal breccias. It is clear that the epithermal gold veins prefer the competent pre-breccia rocks which crack easily and cleanly compared with the diatreme which is incompetent and has poor cracking characteristics. The exceptions are the Ka Opong and Road 17 veins which clearly cut the upper part of the maar volcanics and where test drilling of these veins within the maar rocks has so far located only low grade gold values.
The relationship of the epithermal gold veins and the diatreme in the mine on Level 6 is shown in Figure 6.
To view "Figure 6. Co-O mine Level 6 geology showing the outline of the diatreme breccia, the porphyry-related copper zones and epithermal gold veins from the resource model. Section lines A-A' and B-B' marked," please visit the following link: .
The epithermal quartz veins are dominantly westerly trending and sub-vertical, with lesser 40 to 50 degrees dipping veins. In summary, some of the vein characteristics are:
Fluid inclusion studies on mine vein samples during the year concluded:
Alteration types identified are:
At surface, the mapped alteration shows that the:
The alteration patterns at depth are:
References
Angeles, C.A., 2012. May-June 2012 Progress Report for Philsaga Mining Corporation. Internal Report.
Hagemann, S. & Grignola, S., 2012. Quartz vein textures, fluid inclusion petrography, microthermometry and interpretation of fluid inclusion data from the Co-O Deposit, Mindanao, Philippines. Internal Report.
Sonntag, I. & Hagemann, S., 2010. Geological and Geochemical Evolution of the Central Eastern Mindanao Ridge, Philippines: The Co-O Mine and District, the Borobo Fault Corridor and the Lingig Area. The University of Western Australia Centre for Exploration Targeting. Internal Report.
Standing, J. & Noble, M., 2011. Structural Analysis of the Vein and Fault Achitecture at the Co-O Gold Mine, Mindanao Island, Republic of the Philippines, Medusa Mining Ltd. Internal Report.
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 Non-Executive 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". 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.
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.
ABN: 60 099 377 849
Contacts:
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Medusa Mining Limited
Peter Hepburn-Brown
Managing Director
+61 8 9367 0601
United Kingdom
Fairfax I.S. PLC (Financial Adviser & Broker)
Ewan Leggat/Laura Littley
+44 (0)20 7598 5368
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Datum: 15.08.2012 - 03:06 Uhr
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