17_DMO

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    Loading of the data/conversion

    Demultiplexing

    Editing

    Geometry

    Amplitude correction

    Frequency filter

    Deconvolution

    Velocity analysis

    NMO/DMO-Correction

    Stacking

    Migration

    MeasurementsNavigation

    Printing/storage Printing/storage

    CMP-Sorting Prestack

    PoststackPost-processing

    Pre-Processing

    Basic scheme of the seismic data processing

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    DMO (Dip move-out)

    A seismic processing operation to correct for the fact

    that, for dipping reflections, the traces of a CMP

    gather do not involve a common reflection point.DMO effectively corrects for the reflection-point

    smear that results when reflectors dip.

    Events with various dips stack with the same velocity

    after DMO.

    (DMO can be performed in a number of ways)

    Sheriff, 1991

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    Horizontal Reflector

    CMP = CDP

    CMP CDP

    Dipping Reflector

    CMP = common mid pointCDP = common depth point

    Dip move out (DMO)

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    Loci of reflection points

    Zero offset: coincident

    Source (S) and geophone (G)

    Common offset: offset between

    Source (S) and geophone (G)

    Show possible reflection points for one particular traveltime

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    DMO correction

    NMO:coordinate transformation from A (yn,t) to B (yn,tn)DMO:

    coordinate transformation from B (yn,tn)to C (y0-t0)Zero-offset migration:

    coordinate transformation from C (y0-t0)to D (ym,t)

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    Dip Move out (DMO)

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    Marine line over a salt structure

    Cases of conflicting dip

    Analysis of data without DMO correction

    Analysis of data with DMO correction

    (following pictures are obtained from Yilmaz, 2001)

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    Selected CMP gathers from a 2D marine dataset

    Yilmaz, 2001

    NMO DMO NMO-1

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    Velocity spectrum

    Without DMO correction

    (smearing of data)

    With DMO correction

    Yilmaz, 2001

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    Close-up view of the velocity

    spectrum and CMP gather

    Without DMO correction

    Yilmaz, 2001

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    Close-up view of the velocity

    spectrum and CMP gather

    With DMO correction

    Yilmaz, 2001

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    Velocity field used to stack the CMP gathers

    Without DMO correction With DMO correction

    Yilmaz, 2001With DMO: less smearing: more detailed velocity field

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    NMO correction of DMO corrected gathers

    Without lateral varying and with lateral varying velocityYilmaz 2001

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    Field example of DMO correction

    NMO

    Stacking

    Migration

    DMO NMO-1 NMO

    CMP stack DMO stack

    Migrated CMP stack Migrated DMO stack

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    CMP stack

    and

    DMO stack

    Yilmaz, 2001

    Amplitudes of reflections

    off the flanks of the salt

    have similar amplitude as

    flat events

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    Comparison between

    Migration of

    CMP stack

    andDMO stack

    Yilmaz, 2001

    Amplitudes of reflections

    off the flanks of the salt

    have higher amplitude

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    Time migration of CMP and DMO stack

    Yilmaz 2001