Select the source logs you want to upscale (e.g., Gamma Ray, Porosity, Water Saturation). Choose an averaging method: Best for porosity and water saturation.

Petrel Basics for Geophysical Interpretation | PDF | File Format - Scribd

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High-resolution static models (often containing tens of millions of cells) are typically too computationally heavy for fluid simulators.

Log data samples rock every few inches, but 3D grid cells are often meters thick. You must average these values into the grid cells intersected by the wellbore. Go to .

Convert your interpreted seismic fault segments into structural model faults using the process step.

Define the Coordinate Reference System (CRS): Click , choose the appropriate geographic or projected datum (e.g., WGS84 / UTM Zone 31N), and click Apply . 2. Data Import and Management

Map structural horizons from the fine model to the coarse simulation model. Flow-calculate equivalent directional permeability ( ) to maintain localized transmissibility.

: Frequently check cross-sections using a Intersection Window to verify that property models match up accurately with real well markers.