Right-click on the folders inside the to import your structural assets:
Flatten the display on a regional marker horizon to remove structural tilt and evaluate true depositional thickness variations.
Petrel is grid-centric. A tutorial walks you through creating a that honors faults and horizons. Then comes upscaling well logs—averaging high-resolution log data into each grid cell. This is often the first “aha!” moment: watching your discrete well data populate the entire 3D volume.
Distributing "properties" like porosity and permeability across your grid using geostatistics. 5. Pro-Tip: Use the "Blue Checkmark" petrel tutorial
Located on the left, this tab stores all raw imported data (wells, seismic, horizons, and cultural data).
Before interpreting data, you must configure the project environment. 2.1. Importing Data Import well headers ( WellHeadcap W e l l cap H e a d ), trajectories ( WellPathcap W e l l cap P a t h ), and logs ( ) through File -> Import .
Check the simulation run for material balance errors and refine the model accordingly. Conclusion Right-click on the folders inside the to import
With your data loaded, you can now map the structural framework of your reservoir. Base Mapping and Visualization Open a new ( Home > Insert > 3D Window ).
This tab hosts your structural frameworks, 3D grids, and upscaled properties.
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Create the skeleton of the grid between horizons.
Right-click on the global folder in the Input Pane and select Import (Selection) . Select your file and choose the format: Well headers ( . ) .
8 GB minimum (though 16 GB+ is highly recommended for 3D modeling).
Well A (GR Log) Well B (GR Log) ┌───┐ ┌───┐ │ ├─── [Top Reservoir] ────>│ ├─── [Top Reservoir] │ │ │ │ │ ├─── [Base Reservoir] ───>│ ├─── [Base Reservoir] └───┘ └───┘ Setting Up a Well Section Window
Static models are often too dense (millions of cells) for rapid dynamic simulation runtimes. You must upscale the static grid to a coarser dynamic grid. Grid Upscaling Create a new, coarser 3D grid (e.g., horizontally with thicker vertical layers).