| Maria Eulália Alberton <mariaeul...@gmail.com>: May 26 06:03AM -0700 
 Dear Users,
 
 I'm trying to get a Z-slide in reflectors below the first one, in an attemp
 to reconstruct paleobathymetry. I'd like to know if there's a reccomended
 way to do it, as I tried the manual and automatic way of tracking and it
 doesn't generate an entire horizon to generate the z-values, even in
 parallel reflector. I also tried to apply cosine phase attribute to see if
 the horizon recogniton gets easier, but I still couldn't do it.  In
 attachment is part of my OpendTect screen display.
 
 Thank you so much for your attention,  I look forward for your reply
 
 Best regards,
 Maria Eulália Alberton
 
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    | Paul de Groot <paul.d...@dgbes.com>: May 26 03:32PM +0200 
 Hi Maria,
 
 If I understand you correctly you want to slice through the seismic data
 parallel to the seabed reflector. This can be done in two ways:
 
 1. Right-click on the horizon entry in the tree (or in the scene) and
 select Workflows -> Create Flattened Scene. (Alternatively, you can launch
 this from the Scenes->New[Horizon Flattened]->3D menu.) In the flattened
 scene add a time-slice (or a volume viewer so you can movie-style inspect
 time-slices)
 2. Right-click on the horizon in the tree (or in the scene) and select
 Tools -> Shift ... In the window that pops up select the seismic data and
 Calculate. Now, you can use the slider to inspect the seismic amplitudes
 extracted parallel to the input horizon in the specified time-gate. Note
 that as you slide up and down, the horizon in the tree changes its name to
 reflect the vertical shift. You can save each shifted horizon as a new
 horizon in the database.
 
 Best regards,
 
 Paul.
 
 --
 *Paul de Groot*
 *Special Adviser*
 
 *-----------------------------------------------------------------------------------------------------------------------*
 
 *dGB Earth Sciences*
 Phone: +31 53 4315155
 E-mail: paul.d...@dgbes.com
 Internet: dgbes.com
 *-----------------------------------------------------------------------------------------------------------------------
 *
 
 
 On Mon, May 26, 2025 at 3:10 PM Maria Eulália Alberton <
 
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    | Maria Eulália Alberton <mariaeul...@gmail.com>: May 26 02:16PM -0300 
 Dear Paul,
 
 I'm trying to extract using a reflector parallel to the seabed reflector
 only for testing, but I need to extract the Z-slice in deeper reflectors
 and preferably in the ones I can identify in my interpretation, not only
 parallel ones. I've already tried to use a time slice, but as I need to
 reconstruct a paleosurface, this method isn't so interesting for this
 project. So, I'd like to know if there's a recommended way to do it, since
 when I try to trace the new horizon, it's never available to generate the
 slice.
 
 Thank you so much for your attention and availability,
 Best regards,
 Maria Eulália Alberton
 
 Em seg., 26 de mai. de 2025 às 11:35, Paul de Groot <paul.d...@dgbes.com>
 escreveu:
 
 
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    | Paul de Groot <paul.d...@dgbes.com>: May 26 08:46PM +0200 
 Hi Maria,
 
 It sounds like using a HorizonCube might be the approach you're looking
 for. This creates a dense collection of horizons, each representing a
 paleosurface. You can then examine your data by either slicing through it
 using a 3D HorizonCube slider or by flattening the seismic data based on
 all the horizons within the HorizonCube. This flattened view is known as
 the Wheeler domain, where the vertical axis represents Relative Geologic
 Time. Consequently, time-slicing within the Wheeler domain allows you to
 analyze your data in terms of (relative) geologic time.
 
 To generate a HorizonCube, the initial step involves mapping a framework of
 key horizons. This is typically done using one of OpendTect's
 inversion-based horizon trackers. These trackers are efficient, offer full
 user control, and can track multiple horizons concurrently by minimizing
 the discrepancy between the horizon dip and the seismic dip. After defining
 the framework horizons, the intervals between them are filled with a dense
 set of additional horizons. This infilling process can be guided by a model
 (e.g., proportional, parallel to upper, parallel to lower horizons) or
 driven by the data itself (inversion-based, or tracking the dip-field).
 
 Please note that to utilize these functionalities, you will need licenses
 for OpendTect Pro, the Dip-Steering plugin, the HorizonCube plugin, and the
 SSIS plugin. The SSIS plugin is specifically required if you intend to
 analyze your data within the Wheeler domain.
 
 You can find helpful training videos and webinars on our website that
 demonstrate these workflows. For instance, this training video
 <https://youtu.be/ZDdItreORiQ> illustrates how to track horizons using
 inversion-based algorithms.
 
 I hope this explanation is helpful.
 
 Best regards,
 
 Paul
 --
 *Paul de Groot*
 *Special Adviser*
 
 *-----------------------------------------------------------------------------------------------------------------------*
 
 *dGB Earth Sciences*
 Phone: +31 53 4315155
 E-mail: paul.d...@dgbes.com
 Internet: dgbes.com
 *-----------------------------------------------------------------------------------------------------------------------
 *
 
 
 On Mon, May 26, 2025 at 7:17 PM Maria Eulália Alberton <
 
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