Presentacion TITAN Porfidos

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    TITAN 24 APLICADO A LA EXPLORACIN DE PORFIDOS

    PROFUNDOS EN DIFERENTES AMBIENTES DEEXPLORACIN

    .Leduar Ramayo, Ph. D.

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    Line Length -2400 m

    24 Ex100m d ipoles12 E

    y100m d ipoles25 current stat ions2 Bx/Bymagnetometer si tes

    current electrode (mobile)current electrode (mobile)

    100m

    crosscross--line potential electrode (fixed)line potential electrode (fixed)

    2400m

    inin--line potential electrode (fixed)line potential electrode (fixed)

    2 channel AM2 channel AM

    1 channel AM1 channel AM

    BxBy

    2 ChannelAM

    Battery

    TypicalStationSet-up QUE ES TITAN 24 ?

    BxBy

    RemoteRemoteMagnetometerMagnetometer

    sitesite

    >20 km

    Base magnetometer SiteBase magnetometer Site

    LAN Link to Logging Truck

    50m

    infinity current electrode (fixed)infinity current electrode (fixed)

    >5-10 km

    100m

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    DC resistividad & IP (cargabilidad)

    Se presenta la inversion de los perfilesdesde 0 hasta aproximadamente 750m(dependiendo de el ambiente geolgico)

    Representacin de datos obtenidos por Titan:

    El arreglo standard es de 2.4 km de longitud

    MT Resistividad

    Se presenta la inversion de los perfiles hastaaproximadamente 1 500m

    DC Resistividad

    PW Modelo 2D MT Resistividad

    IP Cargabilidad

    7

    50metros

    1500metros

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    Inversin 2D de unarreglo convencional de

    6 niveles de datos

    Inversin 2D de un arregloTITAN24 de 24 niveles dedatos

    PROFUNDIDAD DE INVESTIGACIN

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    CASOS DE ESTUDIO

    TITAN 24

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    CASO DE ESTUDIO COPPER MOUNTAIN

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    TR sJ i

    GEOLOGA

    Cortesa Copper Mountain Mining Corporation

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    PLANTA IP (200 M) E IMAGEN 3D

    Imagen de IP 3Dmostrando lacontinuidad de lasanomalas enprofundidad

    Cortesa Copper Mountain Mining

    Corporation

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    40 mrad isosuperficie de cargabilidad,

    mirando al NW

    Pit 1 muestra blancospotenciales al Norte,

    Sur y en profundidad

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    Pit 3 posee potencial

    en el Sur, en el

    centro y en

    profundidad.

    40 mrad isosuperficie de cargabilidad,

    mirando al NW

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    Pit 2 la mineralizacin

    ha sido minada

    40 mrad isosuperficie de cargabilidad,

    mirando al NW

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    Virginia Pit parecetener menor

    mineralizacin hacia el

    este y poco potencial

    en profundidad

    40 mrad isosuperficie de cargabilidad,

    mirando al NW

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    Pit 1 el depsito se

    extiende mas de

    1100 m bajo la

    superficie

    40 mrad isosuperficie de cargabilidad,

    mirando al Sur

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    Posible conexin entre Pit 1 y Pit 3

    40 mrad isosuperficie de cargabilidad,

    mirando al Sur

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    Virginia Pit pareciera ser un depsito

    Superficial, no mas de 100 m

    40 mrad isosuperficie de cargabilidad,

    mirando al Sur

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    Zona Este, se extiende

    hasta 400 m

    de profundidad

    Zona mineralizada profunda, comienza a los 1200 m

    40 mrad isosuperficie de cargabilidad,

    mirando al Sur

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    INTERPRETACION

    Cortesa Copper Mountain Mining

    Corporation

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    COPPER MOUNTAIN - RESULTADOS

    Buenos resultados en un ambiente ruidoso Identificacin y delimitacin de targets a gran profundidad Confirmacin del modelo geolgico Mejor intercepto de mineralizacin: 36.3 m con 2.1% Cu,0.1 g/t

    Au, y 22.7 g/t Ag

    Resultados de las perforaciones posibilitaron el financiamiento por$29 Millones de USD y recursos medidos por 163 MT con 0.43 %de Cu

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    Copper Porphyry Experience Kemess Deposit, Northern BC

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    GEOLOGA

    Gossan

    Formacin Toodoggone(jursico temprano)

    Intrusivos Black Lake(jursico temprano-medio)

    Grupo Takla (trisico superior)

    Kemess Norte

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    Modelo geolgo-geofsico

    Barren Geologic Model Mineralized Geologic Model

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    Barren Geologic Model Mineralized Geologic Model

    Upper Pyrit ic sulp hide Zon es (15-25%)

    Cp + Py sulp hides (

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    2d DC Resist iv i ty Forward Model(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    4.6km

    2d DC Resist iv i ty Forward Model(Ti tan Pole-dipole Array A=100m / N=0.5-32.5)

    Barren Model syn thetic Titan Data Porph yry Mod el- syn thetic Titan Data

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    Late Volcanic

    Host Volcanic

    Host Volcanic

    Late Volcanic

    Intrusive

    Intrusive

    Late Volcanic

    Host Volcanic

    Host Volcanic

    Late VolcanicIntrusive Intrusive

    Pyrit ic Zone

    Cp + Py Zone

    ~100-10k

    ohm-m

    Range

    100-10k

    ohm-m

    Range

    100-10k

    ohm-m

    Range

    100-10k

    ohm-m

    Range

    Notice: a) Excellent Similarity betweenFwd & Inverse Models, b) Marked

    Difference between Barren & Mineralizedand c) Well Resolved 2d Images

    Calculated Response

    from Geologic Model

    Below - used as data for

    2d Invers ion Bottom

    Calculated Response

    from Geologic Model

    Below - used as data for

    2d Invers ion Bottom

    Calculated Response

    from 2d Invers ion Model

    Belowus ing d ata from

    2d Forward Above

    Calculated Response

    from 2d Invers ion Model

    Belowusing data from

    2d Forward Above

    This is Predic ted Titan 2d Resist iv i ty

    Image for over Barren Kemess GeologyThis is Predic ted Titan 2d Resist iv i ty

    Image for over Kemess Porphyr ies

    2d Smooth DC Resist iv i ty Inversion(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    2d Smooth DC Resist iv i ty Inversion(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    Barren Model Porphyry Model

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    2d Chargeabi l i ty Forw ard Model(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    4.6km

    2d Chargeabi l i ty Forward Model(Ti tan Pole-dipole Array A=100m / N=0.5-32.5)

    Barren Model Porphyry Model

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    -N=5

    -N=10

    -N=20

    -N=30

    -N=33

    Late Volcanic

    Host Volcanic

    Host Volcanic

    Late Volcanic

    Intrusive

    Intrusive

    Late Volcanic

    Host Volcanic

    Host Volcanic

    Late VolcanicIntrusive Intrusive

    Pyrit ic Zone

    Cp + Py Zone

    0-50 mrad

    Range

    0-50 mrad

    Range

    0-25 mrad

    Range

    0-25 mrad

    Range

    Calculated Response

    from Geologic Model

    Below - used as data for

    2d Invers ion Bottom

    Calculated Response

    from Geologic Model

    Below - used as data for

    2d Invers ion Bottom

    Calculated Response

    from 2d Invers ion Model

    Belowus ing d ata from

    2d Forward Above

    Calculated Response

    from 2d Invers ion Model

    Belowusing data from

    2d Forward Above

    This is Predic ted Titan 2d Resist iv i ty

    Image for over Barren Kemess GeologyThis is Predic ted Titan 2d Resist iv i ty

    Image for over Kemess Porphyr ies

    Notice: a) Excellent Similarity betweenFwd & Inverse Models, b) Marked

    Difference between Barren & Mineralizedand c) Well Resolved 2d Images

    2d Smooth Chargeabi l i ty Inversion(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    2d Smooth Chargeabi l i ty Inversion(Ti tan Pole-dipo le Array A=100m / N=0.5-32.5)

    Synth etic Titan Data

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    UBICACION DE TITAN 24

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    300E 2700E

    Smooth

    UBC 2d DCResist ivity

    Smooth

    UBC 2d IP

    Chargeabil i ty

    300E

    5100ELINE A

    2700E 5100E

    PRELIMINARY

    PRELIMINARY

    PW 2d MT

    (Unrotated)

    Resist ivity

    100N 2500NLINE TC

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    1500

    1400

    1300

    1200

    1100

    1000

    900

    800

    700

    600

    500

    400

    300

    200

    100

    0

    2-D Model pwur-tm2

    Depth(METERS)

    S N

    N 1 E

    |

    150 |250

    |

    350 |450

    |

    550 |650

    |

    750 |850

    |

    950 |1050

    |

    1150 |1250

    |

    1350 |1450

    |

    1550 |1650

    |

    1750 |1850

    |

    1950 |2050

    |

    2150 |2250

    |

    2350 |2450

    METERS

    0 500 1000 1500

    Ohm-M

    100

    150

    220

    320

    460

    680

    1000

    1499.

    2200.

    3200.

    4600.

    6799.

    10000

    14999.

    21999.

    Smooth

    UBC 2d DC

    Resist ivity

    Smooth

    UBC 2d IPChargeabil i ty

    PW (Unro tated)

    2d MT

    Resist ivity

    100N

    PRELIMINARY

    PRELIMINARY

    PRELIMINARY

    LINE TC

    2500N

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    2d Resist ivi ty (ohm -metres)

    PW MT (Unrotated) 2d Resist ivity

    DCIP 2d Smooth Chargeabil i ty DCIP 2d Smoo th Resist ivity

    2d Chargeabi l i ty (mi l l i radians)

    Kemess NorthKemess North

    Kemess North

    TITAN 2D INVERSIONRESULTS IN GOCAD3D EARTH MODEL(View Looking West)

    0 1km

    0 1km

    N

    N

    Kemess BC

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    Kemess , BCTitan 24 (2 spreads) IP results

    700m

    4800m

    New Target (ORA ZONE) Kemess North Offset Zone Kemess North Deposit

    Resultados Verificados Por Perforaciones

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    Northgate Mineral Corporation Press Release July 26 2007

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    Copper Porphyry ExperienceResolution

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    MODELO GEOLGICO

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    Prfido, Copaquire, Chile

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    Prfido, Copaquire, Chile

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    PORFIDO DE COBRE PROYECTO CERRO CHACAY,Chile, Coromining

    Ubicacin de lneas de TITAN24

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    PORFIDO DE COBRE PROYECTO CERRO CHACAY,Chile, Coromining

    Inversin IP 2D

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    Inversin IP 2D

    February 08, 2011Coro Announces 170 Meters at 0.63% Copper from Drilling

    Program at Chacay Property and Exercise of Warrants

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    Argentina

    Los Azules, Minera Andes Taca Taca, Lumina Copper

    Poposa, Terreno Resources

    Rio Grande, Regulus

    Antofaya, Vale

    Chile

    Cerro Chacay, Coromining

    Copaquirre. lnternationalPBX

    Relincho, Teck

    Mexico

    San Rafael, Scorpio

    Titan 24 Latinoamrica 2010 - 2011

    Peru

    El Tesoro, St. Elias

    Cerro Verde, Freeport y

    Buenaventura

    Los Calatos. Minera Hampton

    Rondoni, Volcan

    Yamana, Volcan

    Constancia, Norsemont

    Condestable, Iberian