Uses a ridge-regression method to fit data to a specific, user-defined number of distinct layers. This is best suited for finding sharp structural boundaries, like the contact point between soil and hard bedrock. 3. Equivalence Analysis
Resolves secondary magnetic field decays using central loop, fixed loop, or coincident loop setups. interpex ix1d v350
: Capability to read resistivity well logs from flat ASCII files and interactively reduce them to discreet layers by fitting straight-line segments. Enhanced Modeling Uses a ridge-regression method to fit data to
Generates a model with many thin layers (often 20 to 150) where resistivity varies smoothly with depth. This is ideal when looking for continuous transitions or water tables. This is ideal when looking for continuous transitions
IX1D v350 supports most common DC resistivity arrays, including: Schlumberger Dipole-dipole Pole-dipole Pole-pole 2. Diverse Data Handling (Resistivity & IP)
IX1D v350 enables the generation of smooth models by selecting the number of layers, starting/ending depths, and the starting resistivity.
Handles measurements in PFE, chargeability (msec), or phase (mrad).