dc.contributor.author | Eide, Christian Haug | |
dc.contributor.author | Schofield, Nick | |
dc.contributor.author | Lecomte, Isabelle | |
dc.contributor.author | Buckley, Simon John | |
dc.contributor.author | Howell, John Anthony | |
dc.date.accessioned | 2024-05-13T08:12:54Z | |
dc.date.available | 2024-05-13T08:12:54Z | |
dc.date.created | 2017-10-23T15:59:22Z | |
dc.date.issued | 2018 | |
dc.identifier.issn | 0016-7649 | |
dc.identifier.uri | https://hdl.handle.net/11250/3130004 | |
dc.description.abstract | 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. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | The Geological Society of London | en_US |
dc.title | Seismic interpretation of sill complexes in sedimentary basins: Implications for the sub-sill imaging problem | en_US |
dc.type | Journal article | en_US |
dc.type | Peer reviewed | en_US |
dc.description.version | acceptedVersion | en_US |
dc.rights.holder | Copyright 2018 The Author(s) | en_US |
cristin.ispublished | true | |
cristin.fulltext | postprint | |
cristin.qualitycode | 1 | |
dc.identifier.doi | 10.1144/jgs2017-096 | |
dc.identifier.cristin | 1506963 | |
dc.source.journal | Journal of the Geological Society | en_US |
dc.source.pagenumber | 193-209 | en_US |
dc.relation.project | Norges forskningsråd: 193059 | en_US |
dc.relation.project | Norges forskningsråd: 234152 | en_US |
dc.identifier.citation | Journal of the Geological Society. 2018, 175 (2), 193-209. | en_US |
dc.source.volume | 175 | en_US |
dc.source.issue | 2 | en_US |