polarity in seismic data

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    Phase and Polarity Issues in Modern Seismic Interpretation*

    Alistair Brown1

    Search and Discovery Article #40397 (2009)Posted March 26, 2009

    *Adapted from oral presentation at AAPG International Conference and Exhibition, Cape Town, South Africa, October 26-29, 2008

    1Consulting Reservoir Geophysicist, Allen, TX ([email protected])

    Abstract

    Zero phase is the objective of almost all seismic data processing today and its interpretive benefits are well knowdifficult to achieve. No more than 50% of seismic data achieves zero phase sufficiently closely for its benefits an

    properly enjoyed. Furthermore, 90 degree phase is a remarkably common accident and, if not identified, can caus

    interpretation.

    All interpreters should know how to visually assess the phase and polarity of their data. I regularly meet those wh

    interpretation that the data has a different phase or opposite polarity to what was first thought. In this paper recom

    phase and polarity assessment will be made, and several phase circles will be presented. For zero phase data timeco-located, and many interpretive procedures on modern workstations are based on this fact. For other phases com

    because time and amplitude are in different locations. Suggestions will be offered for handling the all-too-comm

    data.

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    PHASE AND POLARITY

    ISSUES

    INMODERN

    SEISMIC INTERPRETATION

    AAPG CONVENTION CAPE TOWN, SOUTH AFRICA

    26-29 October 2008 by Alistair Brown2008 Alistair Brown

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    NATURAL PAIRING2008 Alistair Brown

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    ZERO PHASE

    GULF OF MEXICO

    GAS SAND

    2008 Alistair Brown

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    BASEMENT

    ZERO PHASE

    OFFSHORE EASTERN CANADA

    2008 Alistair Brown

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    TOP AND BASE

    GAS SAND

    TOP OF

    BASEMENT

    INCREASE IN IMPEDANCE

    IS

    RED

    INCREASE IN IMPEDANCE

    IS

    BLUE

    EUROPEAN

    POLARITY

    AMERICAN

    POLARITY2008 Alistair Brown

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    900

    600

    300

    00

    P

    H

    A

    S

    E

    2008 Alistair Brown

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    ZERO PHASE 900 PHASE

    AND THERE ARE TWO POLARITIES OF EACHCc 2008 Alistair Brown

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    P

    H

    A

    S

    E

    A

    N

    D

    P

    O

    LA

    R

    I

    T

    Y

    A

    S

    S

    ES

    S

    M

    E

    NT

    O

    P

    P

    OR

    T

    U

    N

    IT

    I

    E

    S

    2008 Alistair Brown

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    INTERPRETIVE ASSESSMENT OF

    PHASE AND POLARITY

    EXAMINE CHARACTER OF HIGH AMPLITUDE REFLECTIONS

    RELATE TO GEOLOGIC UNDERSTANDINGONE OR TWO INTERFACES?

    PAY PARTICULAR ATTENTION TO TERMINATIONS

    AND TO UNCONFORMABLE REFLECTIONS

    SEEK CONCENSUS AMONG SEVERAL OBSERVATIONS

    ITS NOT EASY BUT ITS IMPORTANT2008 Alistair Brown

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    2008 Alistair Brown

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    2008 Alistair Brown

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    2008 Alistair Brown

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    2008 Alistair Brown

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    GULF OF MEXICO

    ZERO PHASE EUROPEAN POLARITY2008 Alistair Brown

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    SHALLOW GAS GULF OF MEXICO

    ZERO PHASE

    EUROPEAN POLARITY

    SALT2008 Alistair Brown

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    SHALLOW GAS GULF OF MEXICO

    PHASE = +900

    2008 Alistair Brown

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    MIOCENE GAS GULF OF MEXICO

    PHASE = +9002008 Alistair Brown

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    ITALIAN PLIOCENE FLUID CONTACT

    PHASE = -900

    2008 Alistair Brown

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    IGNEOUS INTRUSIVE ROCK

    ZERO PHASE

    AMERICAN POLARITY2008 Alistair Brown

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    MALAYSIAN CARBONATE BUILDUP

    PHASE +90

    0

    2008 Alistair Brown

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    Dont assume thephase and polarity

    of your data.

    Confirm them with

    interpretive observation.

    2008 Alistair Brown