For a faster way of screening anomalies to confidently interpret your geology, GeoTeric incorporates RMS amplitude calculations in the iso-proportional slicing tool and also allows the creation of a volumetric RMS cube using processes and workflows. Learn more and follow our step by step guide to c...
Validate has been developed as part of a three year project with industry partners and is a forward modelling tool that will help you understand what the colors mean in the RGB Blends.
It allows you to validate your interpretation by:
On demand Webinar - See What's New in GeoTeric 2018.1
GeoTeric’s Master Project functionality allows the user to transfer data from a Master Project containing all key data into a Client Project which can be worked on individually. It also allows for project items such as horizons and faults to be seamlessly transferred between Client Projects.
The Master Project will be available with the release of GeoTeric 2018.1.
With the upcoming release of GeoTeric 2018.1, a variety of enhancements to the Adaptive Interpretation tools will be added. This is in addition to a Master Project option, a Report View and the release of the Validate module.
One of the interpretation enhancements in GeoTeric 2018.1 will be the ability to edit horizons in the Base Map by polygon – either those picked previously in GeoTeric or newly picked in the Base Map. The polygons can be used to fill horizon interpretations or delete them.
GeoTeric allows seamless connectivity to your existing interpretation platform through GeoTeric’s core Interpret module. The links included with GeoTeric are: Link for Petrel1 and the Link to DecisionSpace2. A Link for Paleoscan3 is available as a separate module.
One of the least known features within GeoTeric is the option for importing multiple well deviation files at once. This can be used for rapidly loading data from mature fields that may already have significant well control. This feature is built into the normal well loading process and is easy to use. The key to rapidly loading multiple deviation files is that all files must be in the same directory and must have the same format. Single cell values, such as well name, must be in the same location, and all data must be in the same columns in all files.
GeoTeric’s Adaptive Fault Interpretation is a powerful data driven and interpreter guided method of structural interpretation. Since the Graph Theory algorithm is used by the Adaptive Interpretation System to generate data following results, not many fault sticks are required to generate an accurate fault plane in GeoTeric. This allows for an efficient method of interpretation.
Dip and Azimuth volumes are used in several ways in GeoTeric, from processes such as Noise Cancellation (SO FMH & SO Noise filters) to attribute generation (SO Semblance, SO Dip Derivative, SO Discontinuity, Flexure, etc...). The majority of these filters/attributes have the symbol SO in front of them, indicating they are Structurally Oriented.
As part of GeoTeric’s Data Conditioning workflow, the Spectral Expression Tool is used to shape your spectrum to increase the frequency content in your data in order to improve the vertical resolution of your data.
RGB Blends of Frequency Decomposition results are very powerful in revealing fine details of the subsurface, but the amount of information that can be extracted from such blends depends on which band-limited response magnitude volumes are used as an input. Selection of the right frequencies depends on the interval, amount of detail and objective of the analysis.
This performance release accelerates GeoTeric’s Expression Tools and boosts the data size that is handled effectively by the application.
The Flexure attribute in GeoTeric is a mean curvature attribute, it measures the amount of deformation on a surface. The Flexure attribute is a second order measurement and therefore is not affected by the local orientation of the surface. Where the reflectors are steeply dipping or flat, the Flexure value is very low, the Flexure value will be greatest where the reflectors are deformed, for example at a fault break.