alturas_ccaccapaqui_feb2009.pdf

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· · · · · 600 hectare project in the gold-silver epithermal belt of southern Peru; Intense alunite and silicic alteration typical of high sulfidation epithermal system; Strong gold and silver rock anomalies associated with silicification and sinters During 2007 preliminary surface exploration was completed by Alturas; Excellent road · · · Located 25 kilometers northwest of 0.5 M oz Brea Pampa gold discovery; ; Previous exploration in the 1990´s limited to referential rock sampling and 4 shallow drillholes; High potential for concealed replacement- style gold-silver mineralization; access. Highlights The 600 hectare Ccaccapaqui property is located 460 kilometers southeast of Lima in the department of Ayacucho, within the same belt that hosts major gold-silver epithermal deposits such as Orcapampa, Arcata, Ares, Antapite and Poracota. The 0.5 Moz Brea Pampa gold deposit lies only 25 kilometers to the southeast. Alturas won 100% rights to the Ccaccapaqui claim in a ballot, ahead of a major company that had also staked the claim on the same day. Location and Ownership During the 1990´s various companies explored the extensive areas of hydrothermal alteration anomalies covering the Tertiary volcanic rocks of southern Ayacucho. They include North Limited and Minera Ares, who conducted reconnaisance geological mapping and rock chip geochemical sampling within the area of the existing Ccaccapaqui property. Ares later drilled 4 short diamond drillholes on the property around the year 2000, but the results are not available. Alturas completed 1:5,000 geological mapping and rock chip geochemical sampling over the project during 2007. High level epithermal alteration textures such as siliceous sinters and massive silicification were identified, togther with strong gold and silver anomalies that confirmed earlier results. To date, Alturas has not conducted geophysical studies nor drilling of the property. More recently, a Newmont/ Buenaventura joint venture has defined 0.5 Mozs of economic gold resources at the nearby Brea Pampa project. Exploration History Ccaccapaui is located within the mid- to late- Tertiary volcanic field of southern Peru. Within the project area, lithic tuffs and dacites of the mid Tertiary Tacaza Group are unconformably overlain by massive andesite flows of the late Tertiary Barroso Group, the lower stratigraphic sequence occupying erosional windows in formerly glaciated valleys. The mid-Tertiary Tacaza sequence is intensely hydrothermally altered, with alteration controlled by regional NW-SE and NE-SW structures. Alteration includes intense argillic, alunitic and silicic alteration of the host tuffs and dacites. Banded “sinter” textures, typical of the upper levels of epithermal alteration systems, are present in some areas. Importantly, the upper andesitic volcanic sequence is largely unaltered and unmineralized, forming a post- mineral cover sequence that may mask earlier mineralization. Geology Forward Looking Statements: The information contained in this brochure is based on the due diligence of Alturas Minerals Corp. management. As such it may contain “forward-looking statements”, which are subject to various risks and uncertainties that could cause actual results and future events to differ materially from those expressed or implied by such statements. Investors are cautioned that such statements are not guarantees of future performance and results. Risks and uncertainties about the Company's business are more fully discussed in the Company's disclosure documents filed from time to time with the Canadian securities authorities. CCACCAPAQUI PROJECT (GOLD-SILVER) Ccaccapaqui and major epithermal deposits within a segment of southern Peru Gold-silver -mineralized silicified volcanics in foreground overlain by glacial till in background Glacial till Gold-silver in silicic alteration

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  • 600 hectare project in the gold-silverepithermal belt of southern Peru;

    Intense alunite and silicic alteration typicalof high sulfidation epithermal system;

    Strong gold and silver rock anomaliesassociated with silicification and sinters

    During 2007 preliminary surfaceexploration was completed by Alturas;

    Excellent road

    Located 25 kilometers northwest of 0.5 Moz Brea Pampa gold discovery;

    ;

    Previous exploration in the 1990s limitedto referential rock sampling and 4 shallowdrillholes;

    High potential for concealed replacement-style gold-silver mineralization;

    access.

    Highlights

    The 600 hectare Ccaccapaqui property is located460 kilometers southeast of Lima in thedepartment of Ayacucho, within the same belt thathosts major gold-silver epithermal deposits suchas Orcapampa, Arcata, Ares, Antapite andPoracota. The 0.5 Moz Brea Pampa gold depositlies only 25 kilometers to the southeast.

    Alturas won 100% rights to the Ccaccapaqui claimin a ballot, ahead of a major company that hadalso staked the claim on the same day.

    Location and Ownership

    During the 1990s various companies exploredthe extensive areas of hydrothermal alterationanomalies covering the Tertiary volcanic rocks ofsouthern Ayacucho. They include North Limitedand Minera Ares, who conducted reconnaisancegeological mapping and rock chip geochemicalsampling within the area of the existingCcaccapaqui property. Ares later drilled 4 shortdiamond drillholes on the property around theyear 2000, but the results are not available.

    Alturas completed 1:5,000 geological mappingand rock chip geochemical sampling over theproject during 2007. High level epithermalalteration textures such as siliceous sinters andmassive silicification were identified, togther withstrong gold and silver anomalies that confirmedearlier results. To date, Alturas has not conductedgeophysical studies nor drilling of the property.

    More recently, a Newmont/ Buenaventura jointventure has defined 0.5 Mozs of economic goldresources at the nearby Brea Pampa project.

    Exploration History

    Ccaccapaui is located within the mid- to late- Tertiaryvolcanic field of southern Peru. Within the projectarea, lithic tuffs and dacites of the mid TertiaryTacaza Group are unconformably overlain bymassive andesite flows of the late Tertiary BarrosoGroup, the lower stratigraphic sequence occupyingerosional windows in formerly glaciated valleys.

    The mid-Tertiary Tacaza sequence is intenselyhydrothermally altered, with alteration controlled byregional NW-SE and NE-SW structures. Alterationincludes intense argillic, alunitic and silicic alterationof the host tuffs and dacites. Banded sintertextures, typical of the upper levels of epithermalalteration systems, are present in some areas.

    Importantly, the upper andesitic volcanic sequence islargely unaltered and unmineralized, forming a post-mineral cover sequence that may mask earliermineralization.

    Geology

    Forward Looking Statements: The information contained in this brochure is based on the due diligence of Alturas Minerals Corp.management. As such it may contain forward-looking statements, which are subject to various risks and uncertainties that could causeactual results and future events to differ materially from those expressed or implied by such statements. Investors are cautioned that suchstatements are not guarantees of future performance and results. Risks and uncertainties about the Company's business are more fullydiscussed in the Company's disclosure documents filed from time to time with the Canadian securities authorities.

    CCACCAPAQUI PROJECT(GOLD-SILVER)

    Ccaccapaqui and major epithermal depositswithin a segment of southern Peru

    Gold-silver -mineralized silicified volcanics in foregroundoverlain by glacial till in background

    Glacial till

    Gold-silver

    in silicic alteration

  • Forward Looking Statements: The information contained in this brochure is based on the due diligence of Alturas Minerals Corp.management. As such it may contain forward-looking statements, which are subject to various risks and uncertainties that could causeactual results and future events to differ materially from those expressed or implied by such statements. Investors are cautioned that suchstatements are not guarantees of future performance and results. Risks and uncertainties about the Company's business are more fullydiscussed in the Company's disclosure documents filed from time to time with the Canadian securities authorities.

    Strong gold and silver values are associated withmassive and banded siliceous alteration, andalunite-silica breccias, all of which appear to becontrolled by favourable stratigraphy and the NW-SE and NE-SW structures. In systematic samplingof siliceous outcrops by Alturas (219 samples),values of up to 3.19 g/t gold and 194 g/t silverhave been identified, distributed in a semi-coherent anomaly +1.50 x 0.50 kilometers indimension.

    Distinctive banded chalcedonic sinter depositsoccur in the northwestern part of the prospect andreport spotty gold values of up to 0.76 g/t.

    The results obtained from 4 shallow drillholespreviously completed by Ares are not known. It isworth noting that the earlier holes are only sitedadjacent to outcrops and have not tested beneaththe areas of extensive glacial cover.

    Mineralization

    Strong gold-silver values, associated withsiliceous alteration and breccias, are highlyencouraging. There is excellent potential todiscover concealed zones of bulk tonnage gold-silver mineralization hosted in tuffs along the maincontrolling structures and their intersections.Alturass assessment is that the existing widely-spaced drillholes have not adequately tested thepotential of this kilometric-scale high sulfidationgold-silver system.

    Alturas proposes a detailed geophysicalprogram that would include an electricaltechnique, such as induced polarization, followedby drilling. The company is currently seeking apartner to assist in advancing the project further.

    No systematic geophysics has ever beenconducted on the property, in spite of theextensive glacial cover that could easily maskreplacement-style high sulfidation gold-silvertargets.

    Future Program