INTERPRETATION OF GEOPHYSICAL DATA GRAVITY & MAGNETIC...

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Sustainable Development Goals Short Course IV on Exploration and Development of Geothermal Resources Anna Mwangi (PhD.), Senior Geophysicist, KenGen INTERPRETATION OF GEOPHYSICAL DATA GRAVITY & MAGNETIC METHODS 22/11/2019

Transcript of INTERPRETATION OF GEOPHYSICAL DATA GRAVITY & MAGNETIC...

  • Sustainable Development Goals Short Course IV on Exploration and Development of Geothermal Resources

    Anna Mwangi (PhD.), Senior Geophysicist, KenGen

    INTERPRETATION OF GEOPHYSICAL DATAGRAVITY & MAGNETIC METHODS

    22/11/2019

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    GRAVITY METHOD

    Distance (km)

    Gra

    vity

    (m

    Gal

    s)

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    GRAVITY METHODS

    • Applicable to determine the density distribution in rock units

    • Aim is to map density contrast within rocks

    Method is cost effective and useful in:-

    • Early stage exploration to locate anomalous magma bodies which are central in active geothermal systems

    • Production stage in monitoring of geothermal reservoirs to ensure mitigation measure are used to maintain mass balance in the system.

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    GRAVITY VALUES OLKARIA

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    REGIONAL GRAVITY VALUES CENTRAL RIFT VOLCANOES

    170000 190000 210000 230000 250000

    Eastings(m)

    9860000

    9870000

    9880000

    9890000

    9900000

    9910000

    9920000

    9930000

    No

    rth

    ing

    s(m

    )

    -2200

    -2120

    -2040

    -1960

    -1880

    -1800

    -1720

    -1640

    -1560

    -1480

    SuswaCaldera

    LongonotCaldera

    Olkaria

    g.u.

    0.90S

    1.20S

    36.40

    E36.20

    E

    0 10000 20000 (m)

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    GRAVITY DATA REDUCTION

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    GRAVITY BOUGUER ANOMALIES – OLKARIA DOMES

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    ONGOING OLKARIA PRECISE MONITORING-GRAVITY

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    MAGNETIC METHOD

    • Investigate the magnetic property of rocks

    • Geothermal environment are highly mineralized, mineral deposition along open structures hence magnetic minerals aggregate and hence there will be an increased magnetic field intensity.

    • Useful in early stage exploration to locate geologic structures and

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    MAGNETIC FIELD RESPONSE

    Dyke intrusive magnetic body

    Dep

    th (m

    )

    Magn

    etic field stren

    gth

    (m)

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    TOTAL MAGNETIC INTENSITY - OLKARIA

    (Mariita, 1995)

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    EXAMPLE OF MAGNETIC ANOMALY MAP

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    RESISTIVITY VS GRAVITY INTERPRETATION

    4km depth resistivity slice

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

  • SDG Short Course IV on Exploration and Development of Geothermal ResourcesOrganized by UNU-GTP and KenGen | Lake Bogoria and Lake Naivasha | Nov 14-4 Dec, 2019

    INFORMATION

    Name of course: SDG Short Course IV on Exploration and Development of Geothermal Resources

    Location: Lake Bogoria and Lake Naivasha, Kenya

    Timing: November 14-December 4, 2019

    Organized by: United Nations University Geothermal Training Programme (UNU-GTP) and Kenya Electricity Generating Company PLC (KenGen)

    Financed by: UNU-GTP and KenGen

    Presentation author(s): ([email protected])

    Kenya Electricity Generating Company

    P.O Box 20117, Naivasha, Kenya

    www.kengen.co.ke