Seismic interpretation of sill complexes in sedimentary basins: Implications for the sub-sill imaging problem

• Published in: Journal of the Geological Society
• Main Authors: Eide, Christian Haug, Schofield, Nick, Lecomte, Isabelle, Buckley, Simon John, Howell, John Anthony
• Format: Article in Journal/Newspaper
• Language: English
• Published: The Geological Society of London 2018
• Subjects: Greenland; East Greenland
• Online Access: https://hdl.handle.net/11250/3130004; https://doi.org/10.1144/jgs2017-096

Application of 3D-seismic reflection-data to igneous systems in sedimentary basins has led to a revolution in the understanding of mafic sill-complexes. However, there is considerable uncertainty on how geometries and architecture of sill-complexes within the subsurface relates to those imaged in seismic reflection-data. To provide constraints on how sill-complexes in seismic data should be interpreted, we present synthetic seismograms generated from a seismic-scale (22x0.25 km) outcrop in East Greenland constrained by abundant field-data. This study highlights how overlying igneous rocks adversely affect imaging of underlying intrusions and rocks by decreasing seismic amplitude, frequency and making steeply dipping features near-impossible to image. Furthermore, seismic modelling in this study shows that, because of the high impedance contrast between siliciclastic host-rock and dolerites, very thin (1-5 m) intrusions should in principle be imaged in reflection-seismic data at 3 km depth. However, comparison with actual seismic data with well-data shows significant amounts of un-imaged sill intrusions, and this is likely due to limited seismic resolution, overburden complexity, inadequate velocity-models, and interference between reflections from closely spaced sills and sill-splays. Significant improvements to sill imaging and interpretation could be made by better predicting occurrence and geometry of sill intrusions and including these in velocity models. acceptedVersion