GEOSCIENCE

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moony
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mohammed radwan
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    جاوب واسال

    moony
    moony
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    انثى عدد الرسائل : 77
    Localisation : alexandria
    Emploi : student
    university : alexandria university
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف moony 2007-11-21, 11:24 pm

    both are wave phases results from the energy souce zero phase wavelet is symmetric on the origin and it is produced from vibrosis
    minimum phase is a wave with zero amplitude at the origin it is produced from other sources of energy
    for processing all waves must be in minimum phase
    The minimum phase wavelet has a short time duration and a concentration of energy at the start of the wavelet. It is zero before time zero (causal). An ideal seismic source would be a spike (maximum amplitude at every frequency), but the best practical one would be minimum phase. It is quite common to convert a given wavelet source wavelet into it's minimum phase equivalent since several processing stages (e.g. predictive deconvolution) work best by assuming that the input data is minimum phase. The maximum phase wavelet is the time reverse of the minimum phase and at every point the phase is greater for the maximum than the minimum. All other causal wavelets are strictly speaking mixed-phase and will be of longer time duration. The convolution of two minimum phase wavelets is minimum phase. The zero-phase wavelet is of shorter duration than the minimum phase equivalent. The wavelet is symmetrical with a maximum at time zero (non-causal). The fact that energy arrives before time zero is not physically realisable but the wavelet is useful for increased resolving power and ease of picking reflection events (peak or trough). The convolution of a zero-phase and minimum phase wavelet is mixed phase (because the phase spectrum of the original minimum phase wavelet is not the unique minimum phase spectrum for the new modified wavelet) and should be avoided

    جاوب واسال - صفحة 2 Wavelets

    and now the question is what are the types of core analysis?
    avatar
    takey
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    تاريخ التسجيل : 07/10/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف takey 2007-11-22, 10:20 am

    Excellent answer moony

    lol!
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    takey
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    ذكر عدد الرسائل : 41
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    Emploi : Geophysicist
    university : Mansoura
    تاريخ التسجيل : 07/10/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف takey 2007-11-22, 11:11 am

    The Major Types of Core Analysis

    • Plug (Conventional) Analysis

      • Consolidated Formations
      • UnconsolidatedFormations

    • Full-Diameter Analysis

      • Routine Analysis
      • Pressure Core Analysis
      • Sponge Core Analysis

    • Sidewall Core Analysis

    1. Plug (Conventional) Analysis

    a. Consolidated Formations


    This technique is normally
    restricted to homogeneous formations that can be characterized with plug-size
    samples. Typical plug size is 1 inch (2.5 m) in diameter, and 1 inch (2.5 cm)
    long.

    b. Unconsolidated Formations

    Unconsolidated
    sand recovered within a rubber sleeve core barrel, a plastic inner barrel
    liner, or a fiberglass barrel is often stabilized by freezing prior to
    sampling. Frozen interstitial water present at the grain contacts immobilizes
    the rock particles. Plugs are drilled using liquid nitrogen as the bit
    lubricant.

    2. Full Diameter Analysis
    a. Routine Analysis

    Full
    diameter analysis was introduced to allow testing of rocks with complex
    lithology, such as heterogeneous carbonates and fissured, vugular formations
    unsuitable for plug analysis.

    b. Pressure Core Analysis

    The analysis of full diameter
    pressure cores follows, in a modified form, the procedures normally employed in
    more routine analysis. Full diameter samples are cut in the form of a right
    cylinder and then placed in specialized, airtight containers where they thaw,
    so that fluids expulsed from the core can be collected and measured.

    c. Sponge Core Analysis

    Full diameter analysis of
    samples recovered within the sponge barrel proceeds along the usual lines once
    the core has been removed from the barrel. The sponge itself is cut from the
    core barrel and the fluids it contains are extracted using a vacuum retort
    technique. Both oil and water volumes within the sponge are measured.

    3. Sidewall Core Analysis


    Sidewall samples are used extensively
    in softer sand areas. (Note, however, that a sidewall-drilled plug from a new
    sidewall coring device can be used for harder formations and can be analyzed in
    the same manner as a standard plug-sized core.) Percussion sidewalls are often
    smaller and demand additional attention.



    Now Easy Question



    What is the Ground roll??
    hosny hassan
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    ذكر عدد الرسائل : 68
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    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-11-27, 9:27 pm

    ØSurface waves (often called ground roll) are usually present on reflection records
    ØFor the most part, these are Rayleigh waves with velocities ranging from 100 to 1000 m/s or so.
    ØGround roll frequencies usually are lower than those of reflection and refractions, often with the energy concentrated below 15 Hz.
    ØGround roll alignments are straight, just as refractions are, but represent lower velocities.
    ØGround roll energy generally is high enough even in the reflection band to override all but the strongest reflections.
    ØOccasionally where ground roll is exceptionally strong, in line offsets are used so that desired reflections can be recorded before the surface waves reach the spread.
    bom
    hosny hassan
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-11-27, 9:34 pm

    i hope this answer will be sufficient
    my next question
    what is Dip moveout processing?
    thank u takey about this answer
    Question
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    takey
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    ذكر عدد الرسائل : 41
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    university : Mansoura
    تاريخ التسجيل : 07/10/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف takey 2007-12-02, 1:00 am




    A
    traveltime curve resulting from a dipping reflector has two velocity
    components. The first component is the normal moveout component, which is a
    factor of the geometry of the seismic array and the increasing distance from
    the zero offset location to the far receivers. The second component is caused
    by the presence of structural dip.



    This
    second component is reflected in the asymmetry of the travel paths on either
    side of the zero offset location. Travel paths on the updip side have shorter
    raypaths and, therefore, faster traveltimes than those on the downdip side.
    This phenomenon is most apparent with shot gather data, but it also occurs on a
    smaller scale with CMP gather data.



    The first velocity component is taken into account by
    applying a normal move-out (NMO) correction. The second is handled by
    applying a dip moveout (DMO) correction.






    While NMO corrects for the time
    delay on an offset trace by moving the amplitudes to earlier times on the trace,
    DMO moves the data up-dip to the correct position where a zero-offset trace
    would record a dipping reflector (Figure 1). Migration then moves the energy to
    the correct horizontal and vertical subsurface location.


    Image hosted by servimg.com
    Fig. 1. Data movement during NMO, DMO, and
    migration (after Sheriff, 1991).
    Image hosted by servimg.com


    Figure 2 and Figure 3 are
    an example of data in a highly faulted area. In this case, DMO improves the
    data quality. In Figure 2 , the arrows point to a reflector that appears to be
    fairly continuous. But in Figure 3 , we can see that the reflector is faulted
    and that DMO has improved the overall fault definition in this area



    Finally, we can say that the DMO “Dip MoveOut”
    is A geophysical process which corrects for differences in arrival times at
    different geophone offset positions caused by the dip of a reflector.





    Now what do u know about (OBC) ocean-bottom cable?

    scratch
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-12-02, 5:52 am

    weeeeeeeehaa very nice takey
    thank u very much
    really really really thanks
    the answer of your question is ready
    Smile
    hosny hassan
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-12-02, 6:45 am

    Ocean Bottom Seismograph (OBS)
    جاوب واسال - صفحة 2 Clip_310
    In the 1990s, the introduction of Ocean Bottom Cable (OBC), where the seismic cables are laid down on the sea bottom
    A particular kind of OBC includes two seismic sensors, one hydrophone and one multicomponent receiver. The hydrophone provides pressure measurements while the multicomponent receiver, which consists of three geophones oriented in directions perpendicular to each other, measures the components of the elastic wavefield.
    ØThis particular seismic acquisition method, known as Ocean Bottom Seismograph (OBS), yields satisfactory data quality for S-wave energy in a marine environment.
    ØMulticomponent seismic surveys record both P-waves and shear, or S-waves; this is achieved by recording all components of the returning wavefield.
    ØEach sensor within a multicomponent recording cable comprises three orthogonally oriented geophones for land acquisition, plus a hydrophone for marine acquisition (hence four-component or 4C).
    ØP-waves are detected primarily by the Z-component geophone and the hydrophone, while S-waves are detected primarily by the X- and Y-component geophones.
    ØThe 3C data can then be used to “create” the shear wave mode, called a C-wave, by converting the S-wave signal using a P-to-S mode conversion algorithm technique
    .
    جاوب واسال - صفحة 2 Clip10
    جاوب واسال - صفحة 2 Clip_210
    4-C sensor
    ØBecause of the nature of the OBS data acquisition, combining the vertical component (Z-component) of the vector wavefield and the pressure component (hydrophone), a process known as PZ summation, produces PZ seismic sections, which are ideally free of water-bottom multiples
    جاوب واسال - صفحة 2 Clip_411
    جاوب واسال - صفحة 2 Clip_510
    ØThe PS sections of the OBS seismic dataset have proved to be useful in several areas, as for example, the identification of gas seepages, P-wave reflections are disturbed by the presence of gas in the subsurface, however, S-waves help to clarify the subsurface image since they are not affected by the presence of gas.

    جاوب واسال - صفحة 2 Clip_610
    جاوب واسال - صفحة 2 Clip_710

    cyclops bounce














    عدل سابقا من قبل في 2007-12-02, 7:29 am عدل 1 مرات
    hosny hassan
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-12-02, 6:47 am

    i hope this will help you
    i find it great to answer many questions to get more information
    this is really good partition in the forum
    thanks takey about the question
    pirat
    hosny hassan
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-12-02, 6:55 am

    now my question is
    what is the concept of seismic stratigraphy and its applications in determining the real lithology ?
    Idea
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    takey
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    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف takey 2007-12-02, 11:05 am

    Exxxxxcellent answer my Friend Hossny


    انتا ديما يا حسنى عند حسن الظن
    hosny hassan
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    ذكر عدد الرسائل : 68
    العمر : 37
    Localisation : alexandia, egypt
    university : geophysics departement
    تاريخ التسجيل : 12/09/2007

    جاوب واسال - صفحة 2 Empty رد: جاوب واسال

    مُساهمة من طرف hosny hassan 2007-12-03, 9:23 pm

    thanks for your kindness
    really thanks
    انا اجي ايه جنب سعتك
    شكرا مرة تانية
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