| OpendTect dGB Plugins User Documentation version 3.2 | ||
|---|---|---|
| Prev | Chapter 3. Sequence Stratigraphic Interpretation System | Next |


There are five models available to calculate the chronostratigraphy. 
SSIS Models
Three models are based on interpolation and one model uses a data driven approach:
Linear Interpolation: Linear interpolation can also be used for 3D Stratal Slicing or Proportional Slicing. If this model is selected, the user can specify the spacing between two chronostrat-horizons.
Parallel to upper: This model best depicts the lapout patterns for instance onlaps. In settings the user can specify vertical spacing between chronostrat-horizons.
Parallel to lower: This model relates to upward truncation patterns. In settings the user can specify vertical spacing between chronostrat-horizons.
Data driven: This model is driven from data based upon steering information. The chronostratigraphy will follow the dip and azimuth information.

Event Driven: This model drives the chronostratigraphy by following the events. If you press settings, you can select the (event) phases to use: Max/Min Only, Zero Crossing Only, or Max/Min and Zero Crossing. The tracked chronostratigraphy will be the combination of selected phases.





directly. It will allow to slide the chrono-horizons from top to bottom or vice versa. This is a key tool of SSIS in analyzing and identifying the stratigraphic surfaces.
| Prev | Home | Next |
| Data Preparation | Up | Wheeler Transform / Wheeler Scene |