Mapping horizons and fracture patterns in coal measures using magnetics for coalbed methane exploration in Queensland

Abstract

High resolution magnetic data has successfully been used to map the top and base of coal measures, related faults and fracture patterns across the Red Hill area in the northern Bowen Basin, eastern Australia. A horizon mapping technique, based on energy spectral analysis (ESA), was used to detect magnetic susceptibility contrasts that were laterally merged to form two magnetic interfaces, corresponding to the top of the Fair Hill Formation and base of the Goonyella Middle Seam in the Permian Moranbah coal measures. The depth estimates were made at stations on a regular mesh of 400 m x 400 m and at nine wells. The final detailed mapping of both horizons was constructed from spectral depth estimates on a regular mesh of 100 m x 100 m. Major faults, associated structures and fractures were mapped in 3D from the magnetic data by using automatic curve matching (ACM). This technique was applied to detect single magnetic anomalies produced by inter-sedimentary sources. These results were used to interpret magnetic lineaments in, above and below the coal measures to produce a rock fabric model. The results obtained from the interpretation of the magnetic data are consistent with structures mapped from existing seismic and well data. The mapped rock fabric was also confirmed by well results to be a fair representation of the open fracture set, which has an orientation that is consistent with the existing stress regime.

Mapping sub-volcanic geology using magnetic data

“…This magnetic field was subtracted from the TMI data and the resultant magnetic field of the sub-volcanic crust was computed (Figure 8). Such a resultant magnetic field, if computed over a sedimentary basin, can be further analysed and interpreted using the Horizon Mapping technique discussed in Kivior et al, 2015 and2018. This would allow mapping of multiple sub-volcanic sedimentary horizons and structures.…”