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1.0pt+ADs- mso-border-alt:solid windowtext .5pt+ADs-padding:0cm'+AD4-ASX RELEASE+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADsAJg-nbsp+ADs- +ADw-/span+AD4-17 JUNE 2009+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal align+AD0-center style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt: auto+ADs-text-align:center+ADs-line-height:150+ACU-'+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-span style+AD0-'font-size:14.0pt+ADs-line-height:150+ACUAOw-font-family:Georgia+ADs-border:solid windowtext 1.0pt+ADs- mso-border-alt:solid windowtext .5pt+ADs-padding:0cm'+AD4APA-br+AD4- +ADw-/span+AD4APA-/b+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-u+AD4APA-span style+AD0-'font-size: 20.0pt+ADs-line-height:150+ACUAOw-font-family:Georgia+ADs-mso-fareast-language:ZH-HK'+AD4-MINERALOGY CONFIRMED AT MARENICA URANIUM PROJECT+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/u+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-International uranium company West Australian Metals Limited (ASX: +ADw-b style+AD0-'mso-bidi-font-weight: normal'+AD4-WME+ADw-/b+AD4-) is pleased to advise that it has received encouraging preliminary results from mineralogical+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADs- +ADw-/span+AD4-test work on ore samples from its 80+ACU--owned +ADw-b style+AD0-'mso-bidi-font-weight: normal'+AD4-Marenica Uranium Project+ADw-/b+AD4- in Namibia. +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-International consultancy group SRK Consulting Pty Ltd collected a full suite of samples for mineralogy and verification process test work whilst on site in May. Three styles of mineralization have been delineated on site by SRK, namely:+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-ul type+AD0-disc+AD4- +ADw-li class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify+ADs-mso-list:l0 level1 lfo1+ADs-tab-stops:list 36.0pt'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-a primary source+ADsAPA-/span+AD4- +ADw-span style+AD0-'font-family: Georgia'+AD4APA-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/li+AD4- +ADw-li class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify+ADs-mso-list:l0 level1 lfo1+ADs-tab-stops:list 36.0pt'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-an oxidized source in bedrock (secondary)+ADs- and +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/li+AD4- +ADw-li class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify+ADs-mso-list:l0 level1 lfo1+ADs-tab-stops:list 36.0pt'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-calcrete-hosted uranium mineralization. +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/li+AD4- +ADw-/ul+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia'+AD4-To date, 30 sections of Marenica ore have been examined ? two primary, 19 secondary and surface rocks and nine calcrete.+ACY-nbsp+ADs-In the calcrete and secondary ores the major uranium phase is carnotite (in the order of 85+ACU- or more). Based on this analysis, SRK confirm that the material described in the previously produced AMMTEC report (2008) is not representative of the mineralogy observed in samples collected on site.+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4-Based on the mineralogy of the ores collected to date and comparisons with other uranium ores from Africa, SRK believes that WME +ADw-b style+AD0-'mso-bidi-font-weight:normal'+AD4-should be able to achieve better than 75+ACU- extraction+ADw-/b+AD4- from supergene ore types.+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-u+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4-Calcrete Mineralisation+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/u+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4-Uranium occurs in calcrete in-filling fractures and as fine grained coatings on granite pebble fragments and in the surface gypcrete. The mineralisation occurs with a host of gangue minerals including calcite, Sr-Mg-calcite, celestine, gypsum, halite, mirabilite, etc. +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4-Most rock fragments are angular implying little lateral movement, suggesting that they occur+ACY-nbsp+ADs-close to the source. The major mineral present is carnotite (K+ADw-sub+AD4-2+ADw-/sub+AD4-(UO+ADw-sub+AD4-2+ADw-/sub+AD4-)+ADw-sub+AD4-2+ADw-/sub+AD4AWw-VO+ADw-sub+AD4-4+ADw-/sub+AD4AXQ-.3H+ADw-sub+AD4-2+ADw-/sub+AD4-O). In addition to this there are minor amounts of urancalcarite (Ca(UO+ADw-sub+AD4-2+ADw-/sub+AD4-)+ADw-sub+AD4-3+ADw-/sub+AD4AWw-(OH)+ADw-sub+AD4-6+ADw-/sub+AD4-(CO+ADw-sub+AD4-3+ADw-/sub+AD4-)+AF0-.3H+ADw-sub+AD4-2+ADw-/sub+AD4-O) and rutherfordine (UO+ADw-sub+AD4-2+ADw-/sub+AD4-(CO+ADw-sub+AD4-3+ADw-/sub+AD4-)). +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APAAh---+AFs-if gte vml 1+AF0APgA8-v:shapetype id+AD0AIgBf-x0000+AF8-t75+ACI- coordsize+AD0AIg-21600,21600+ACI- o:spt+AD0AIg-75+ACI- o:preferrelative+AD0AIg-t+ACI- path+AD0AIg-m+AEA-4+AEA-5l+AEA-4+AEA-11+AEA-9+AEA-11+AEA-9+AEA-5xe+ACI- filled+AD0AIg-f+ACI- stroked+AD0AIg-f+ACIAPg- +ADw-v:stroke joinstyle+AD0AIg-miter+ACI-/+AD4- +ADw-v:formulas+AD4- +ADw-v:f eqn+AD0AIg-if lineDrawn pixelLineWidth 0+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-sum +AEA-0 1 0+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-sum 0 0 +AEA-1+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-2 1 2+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-3 21600 pixelWidth+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-3 21600 pixelHeight+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-sum +AEA-0 0 1+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-6 1 2+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-7 21600 pixelWidth+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-sum +AEA-8 21600 0+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-prod +AEA-7 21600 pixelHeight+ACI-/+AD4- +ADw-v:f eqn+AD0AIg-sum +AEA-10 21600 0+ACI-/+AD4- +ADw-/v:formulas+AD4- +ADw-v:path o:extrusionok+AD0AIg-f+ACI- gradientshapeok+AD0AIg-t+ACI- o:connecttype+AD0AIg-rect+ACI-/+AD4- +ADw-o:lock v:ext+AD0AIg-edit+ACI- aspectratio+AD0AIg-t+ACI-/+AD4- +ADw-/v:shapetype+AD4APA-v:shape id+AD0AIg-Picture+AF8-x0020+AF8-3+ACI- o:spid+AD0AIgBf-x0000+AF8-s1027+ACI- type+AD0AIgAjAF8-x0000+AF8-t75+ACI- style+AD0-'position:absolute+ADs-left:0+ADs-text-align:left+ADs-margin-left:0+ADs-margin-top:0+ADs- width:486pt+ADs-height:324pt+ADs-z-index:1+ADs-visibility:visible'+AD4- +ADw-u1:wrap type+AD0AIg-topandbottom+ACIAPgA8-/u1:wrap+AD4- +ADw-/v:shape+AD4APAAhAFs-endif+AF0---+AD4APAAhAFs-if +ACE-vml+AF0APgA8-img width+AD0-648 height+AD0-432 src+AD0AIg-20090617434784+AF8-fichiers/image001.gif+ACI- v:shapes+AD0AIg-Picture+AF8-x0020+AF8-3+ACIAPgA8ACEAWw-endif+AF0APgA8-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4APA-o:p+AD4AJg-nbsp+ADsAPA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-br style+AD0-'mso-ignore:vglayout' clear+AD0-ALL+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto'+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU+ADs-mso-no-proof:yes'+AD4-Micrograph +ADw-/span+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4APA-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-i style+AD0-'mso-bidi-font-style:normal'+AD4APA-span style+AD0-'font-size:10.0pt+ADs-font-family:Georgia'+AD4-This photomicrograph is from core MARD031 at 6.52m and shows a carnotite nugget and veinlet in oxide weathered granite matrix. Field of view is 5mm and the image was taken in plane polarised transmitted light.+ADw-/span+AD4APA-/i+AD4APA-i style+AD0-'mso-bidi-font-style:normal'+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4APA-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/i+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-u+AD4APA-span style+AD0-'font-family:Georgia+ADs-mso-fareast-language:EN-AU'+AD4-Secondary Mineralisation+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/u+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language: EN-GB+ADs-mso-fareast-language:EN-AU'+AD4-Uranium occurs in veinlets and joint surfaces and along fractures with calcite, clays, gypsum, hematite, and siderite.+ACY-nbsp+ADs-Uranium also occurs as uranium (VI) minerals as components of quartz veins in granite matrix that is characterized by intense hematite-siderite alteration and mottled clay alteration of feldspars. +ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language: EN-GB+ADs-mso-fareast-language:EN-AU'+AD4-Uranium mineralogy is dominated again by carnotite (K+ADw-sub+AD4-2+ADw-/sub+AD4-(UO+ADw-sub+AD4-2+ADw-/sub+AD4-)+ADw-sub+AD4-2+ADw-/sub+AD4AWw-VO+ADw-sub+AD4-4+ADw-/sub+AD4AXQ-.3H+ADw-sub+AD4-2+ADw-/sub+AD4-O) together with (minor) fourmarierite (PbU+ADw-sub+AD4-4+ADw-/sub+AD4-O+ADw-sub+AD4-13+ADw-/sub+AD4-.4H+ADw-sub+AD4-2+ADw-/sub+AD4-O) and metatyuyamunite (Ca(UO+ADw-sub+AD4-2+ADw-/sub+AD4-)+ADw-sub+AD4-2+ADw-/sub+AD4AWw-VO+ADw-sub+AD4-4+ADw-/sub+AD4AXQA8-sub+AD4-2+ADw-/sub+AD4-.3-5H+ADw-sub+AD4-2+ADw-/sub+AD4-O).+ACY-nbsp+ADs- An unknown U-Mo-oxide phase has also been identified. In the granite fragments uranium is present as uraninite (UO+ADw-sub+AD4-2+ADw-/sub+AD4-) and as a trace element in xenotime, zircon and monazite.+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-u+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language:EN-GB+ADs-mso-fareast-language:EN-AU'+AD4-Primary Mineralisation+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/u+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language: EN-GB+ADs-mso-fareast-language:EN-AU'+AD4-The two samples examined to date+ACY-nbsp+ADs-from the Phillipus and eastern zones+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADs- +ADw-/span+AD4-have confirmed the presence of primary uranium (IV) mineralization in the granites of the Marenica Licence area. To date the uranium minerals identified are uraninite (UO+ADw-sub+AD4-2+ADw-/sub+AD4-) and euxenite ((Y,Ca,Ce,U,Th)(Nb,Ta,Ti)+ADw-sub+AD4-2+ADw-/sub+AD4-O+ADw-sub+AD4-6+ADw-/sub+AD4-) along with minor amounts of uranium associated with xenotime, zircon and monazite+ADw-/span+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language:EN-GB'+AD4APA-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-b style+AD0-'mso-bidi-font-weight:normal'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language:EN-GB'+AD4-Notes+ADw-o:p+AD4APA-/o:p+AD4APA-/span+AD4APA-/b+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language: EN-GB'+AD4APA-o:p+AD4AJg-nbsp+ADsAPA-/o:p+AD4APA-/span+AD4APA-/p+AD4- +ADw-p class+AD0-MsoNormal style+AD0-'mso-margin-top-alt:auto+ADs-mso-margin-bottom-alt:auto+ADs- text-align:justify'+AD4APA-span lang+AD0-EN-GB style+AD0-'font-family:Georgia+ADs-mso-ansi-language: EN-GB'+AD4-Information in this report that relates+ADw-b style+AD0-'mso-bidi-font-weight: normal'+AD4- to exploration results and laboratory testwork+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADs- +ADw-/span+AD4-currently being collected at Cardiff University,+ADw-/b+AD4- Wales and reflects information compiled by+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADs- +ADw-/span+AD4APA-i style+AD0-'mso-bidi-font-style:normal'+AD4-Eur.Geol.+ADw-/i+AD4- Robert Bowell PhD, C.Chem., C.Geol., Principal Geochemist of SRK Consulting (UK) Limited who has sufficient experience+ADw-span style+AD0-'mso-spacerun:yes'+AD4AJg-nbsp+ADs- +ADw-/span+AD4-relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is reporting on as a Competent Person as defined in the 2004 Edition of ?The Australian Code for Reporting Exploration Results, Mineral Resources and Ore Reserves.? 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