4.6 Article

Evidencing subtle faults in deep seismic reflection profiles: Data pre-conditioning and seismic attribute analysis of the legacy CROP-04 profile

Journal

FRONTIERS IN EARTH SCIENCE
Volume 11, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2023.1119554

Keywords

seismic reflection; legacy data; pre-conditioning filters; seismic attributes; normal faults; earthquakes; seismotectonics; Irpinia 1980 earthquake

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The legacy seismic reflection data have great value for basic research, especially in seismically hazardous areas. Modern tools, such as pre-conditioning techniques and seismic attributes, can effectively improve the data quality and resulting image. In this study, a workflow including pre-conditioning and extraction of seismic attributes is used to improve the quality of CROP-04 deep seismic reflection profile in the Southern Apennines mountain range. The results demonstrate the capacity of this method to extract seismic fabrics and identify fault sets, which can be useful in seismotectonic studies of other high-hazard regions.
Legacy seismic reflection data constitute infrastructure of tremendous value for basic research. This is especially relevant in seismically hazardous areas, as such datasets can significantly contribute to the seismotectonic characterization of the region. The quality of the data and the resulting image can be effectively improved by using modern tools, such as pre-conditioning techniques and seismic attributes. The latter are extensively used by the hydrocarbon exploration industry, but are still only poorly applied to the study of active faults. Pre-conditioning filters are effective in removing random noise, which hampers the detection of subtle geologic structures (i.e., normal faults). In this study, a workflow including pre-conditioning and extraction of seismic attributes is used to improve the quality of the CROP-04 deep seismic reflection profile. CROP-04 was acquired in the 1980s across the Southern Apennines mountain range, one of the most hazardous seismically active regions in Italy. The results show the capacity of this method to extract, from low-resolution legacy data, subtle seismic fabrics that correspond to a dense network of fault sets. These seismic signatures and the enhanced discontinuities disrupting the reflections, which were invisible in the original data, correlate well with the main regional normal faults outcropping at the surface. Moreover, the data reveal higher structural complexity, due to many secondary synthetic and antithetic structures, knowledge of which is useful in modeling of the local and regional distribution of the deformation and potentially in guiding future field mapping of active faults. This proposed approach and workflow can be extended to seismotectonic studies of other high-hazard regions worldwide, where seismic reflection data are available.

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