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  • 1
    Online-Ressource
    Online-Ressource
    Wiley ; 2020
    In:  Near Surface Geophysics Vol. 18, No. 1 ( 2020-02), p. 23-37
    In: Near Surface Geophysics, Wiley, Vol. 18, No. 1 ( 2020-02), p. 23-37
    Kurzfassung: High‐frequency multichannel seismic systems provide detailed images of the shallow marine subsurface. In order to exploit the redundancy inherent in such data optimally, traveltime corrections need to account for normal moveout and static effects due to vertical source and receiver variations. Misalignment of reflections in common‐midpoint gathers will significantly lower the frequency content in the final stack, making this correction particularly important for very high‐frequency seismic data. Traditionally, normal moveout correction involves labour‐intensive picking of stacking velocities, while static corrections can be, by some techniques, performed automatically. In this paper, we present a high‐frequency seismic case study from the Baltic Sea, using seismic image matching as a novel, fully automated technique to perform joint moveout and static corrections. Our multichannel test profiles were acquired offshore Rügen island for wind farm development. Owing to the regular passage of up to 1.5 m high ocean waves during data acquisition, these boomer profiles suffer from strong static effects. We perform joint normal moveout and static corrections by defining the nearest common offset section as a fixed reference frame and minimizing its difference in traveltime with respect to all available common offset sections. Time shifts are computed independent of a pre‐defined traveltime curve, using the normalized cross‐correlation as a measure of data similarity while penalizing irregular displacements by a regularization term. Time shifts are converted to stacking velocities based on the traditional hyperbolic traveltime equation. Our results are compared with those derived by conventional manual velocity analysis and subsequent trim static corrections. We find that image matching produces stacks of similar quality and stacking velocity models of similar to slightly better quality compared with the conventionally derived ones, revealing the potential of this technique to automatize and significantly speed up this first part of the seismic processing chain.
    Materialart: Online-Ressource
    ISSN: 1569-4445 , 1873-0604
    URL: Issue
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2020
    ZDB Id: 2247665-9
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2018
    In:  Marine Geology Vol. 406 ( 2018-12), p. 177-192
    In: Marine Geology, Elsevier BV, Vol. 406 ( 2018-12), p. 177-192
    Materialart: Online-Ressource
    ISSN: 0025-3227
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2018
    ZDB Id: 1500648-7
    ZDB Id: 2181-7
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    Copernicus GmbH ; 2023
    In:  Safety of Nuclear Waste Disposal Vol. 2 ( 2023-09-06), p. 141-141
    In: Safety of Nuclear Waste Disposal, Copernicus GmbH, Vol. 2 ( 2023-09-06), p. 141-141
    Kurzfassung: Abstract. The German site selection procedure for a repository site for high-level nuclear waste is subdivided into three major phases. During the first phase, the subsurface of Germany is evaluated based on existing data, with the aim of defining siting regions for surface-based underground exploration. Although Germany is covered by large amounts of geoscientific data – including ca. 50 000 boreholes deeper than 300 m and more than 340 000 km of reflection seismic lines – the legal obligation to make these data publicly available on a national scale is fairly new and dates back to the Geological Data Act of 2020 (GeolDG: Geologiedatengesetz vom 19. Juni 2020; BGBl. I S. 1387). However, significant amounts of data are available in analogue form only, posing a significant challenge to the timeline of the site selection procedure. As the German nuclear waste management organisation, the Federal Company for Radioactive Waste Disposal (BGE) is in charge of collecting, interpreting and publishing geoscientific data that are relevant to the decisions made within the site selection procedure. In this contribution, we outline the path of data within the first phase of the site selection procedure. We start with an overview of the BGE's current and past activities related to data collection and digitisation, focussing on a major campaign through which more than 16 000 drilling reports are being digitised in cooperation with the State Office for Mining, Energy and Geology in Lower Saxony (LBEG). We then report on the different approaches of data quality control, processing and supply, highlighting challenges related to the federal organisation of geodata storage in Germany. We present selected examples of how data are used for evaluating the subsurface in terms of suitability as a potential repository site. Finally, we give an outlook of how data could be integrated into a web application that is currently being developed as an interactive tool for the public presentation of results and underlying decisions.
    Materialart: Online-Ressource
    ISSN: 2749-4802
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2023
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    Society of Exploration Geophysicists ; 2018
    In:  GEOPHYSICS Vol. 83, No. 3 ( 2018-05-01), p. V171-V183
    In: GEOPHYSICS, Society of Exploration Geophysicists, Vol. 83, No. 3 ( 2018-05-01), p. V171-V183
    Kurzfassung: Stacking of multichannel seismic reflection data is a crucial step in seismic data processing, usually leading to the first interpretable seismic image. Stacking is preceded by traveltime correction, in which all events contained in a common-midpoint (CMP) gather are corrected for their offset-dependent traveltime increase. Such corrections are often based on the assumption of hyperbolic traveltime curves, and a best fit hyperbola is usually sought for each reflection by careful determination of stacking velocities. However, assuming hyperbolic traveltime curves is not accurate in many situations, e.g., in the case of strongly curved reflectors, large offset-to-target-ratios, or strong anisotropy. Here, we found that an underlying model parameterizing the shape of the traveltime curve is not a strict necessity for producing high-quality stacks. Based on nonrigid image-matching techniques, we developed an alternative way of stacking, both independent of a reference velocity model and any prior assumptions regarding the shape of the traveltime curve. Mathematically, our stacking operator is based on a variational approach that transforms a series of seismic traces contained within a CMP gather into a common reference frame. Based on the normalized crosscorrelation and regularized by penalizing irregular displacements, time shifts are sought for each sample to minimize the discrepancy between a zero-offset trace and traces with larger offsets. Time shifts are subsequently exported as a data attribute and can easily be converted to stacking velocities. To demonstrate the feasibility of this approach, we apply it to simple and complex synthetic data and finally to a real seismic line. We find that our new method produces stacks of equal quality and velocity models of slightly better quality compared with an automated, hyperbolic traveltime correction and stacking approach for complex synthetic and real data cases.
    Materialart: Online-Ressource
    ISSN: 0016-8033 , 1942-2156
    RVK:
    Sprache: Englisch
    Verlag: Society of Exploration Geophysicists
    Publikationsdatum: 2018
    ZDB Id: 2033021-2
    ZDB Id: 2184-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2011
    In:  Marine Geology Vol. 284, No. 1-4 ( 2011-6), p. 28-39
    In: Marine Geology, Elsevier BV, Vol. 284, No. 1-4 ( 2011-6), p. 28-39
    Materialart: Online-Ressource
    ISSN: 0025-3227
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2011
    ZDB Id: 1500648-7
    ZDB Id: 2181-7
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    In: Marine and Petroleum Geology, Elsevier BV, Vol. 67 ( 2015-11), p. 368-388
    Materialart: Online-Ressource
    ISSN: 0264-8172
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2015
    ZDB Id: 1494910-6
    ZDB Id: 48427-1
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    In: Marine and Petroleum Geology, Elsevier BV, Vol. 77 ( 2016-11), p. 526-534
    Materialart: Online-Ressource
    ISSN: 0264-8172
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2016
    ZDB Id: 1494910-6
    ZDB Id: 48427-1
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2018
    In:  Engineering Fracture Mechanics Vol. 202 ( 2018-10), p. 116-134
    In: Engineering Fracture Mechanics, Elsevier BV, Vol. 202 ( 2018-10), p. 116-134
    Materialart: Online-Ressource
    ISSN: 0013-7944
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2018
    ZDB Id: 2012718-2
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Online-Ressource
    Online-Ressource
    Wiley ; 2016
    In:  Basin Research Vol. 28, No. 5 ( 2016-10), p. 569-597
    In: Basin Research, Wiley, Vol. 28, No. 5 ( 2016-10), p. 569-597
    Kurzfassung: Messinian evaporites of locally more than 3‐km thickness occupy the subduction zone between Cyprus and Eratosthenes Seamount. Based on a dense grid of seismic reflection profiles, we report on compressional salt tectonics and its impact on the Late Miocene to Quaternary structural evolution of the Cyprus subduction zone. Results show that evaporites have experienced significant post‐Messinian shortening along the plate boundary. Shortening has initiated allochthonous salt advance between Cyprus and Eratosthenes Seamount, representing an excellent example of salt which efficiently escapes subduction and accretion. Further east, between Eratosthenes Seamount and the Hecataeus Rise, evaporites were compressionally inflated without having advanced across post‐Messinian strata. Such differences in the magnitude of salt tectonic shortening may reflect a predominately north–south oriented post‐Messinian convergence direction, raising the possibility of a later coupling between the motion of Cyprus and Anatolia than previously thought. Along the area bordered by Cyprus and Eratosthenes Seamount a prominent step in the seafloor represents the northern boundary of a controversially debated semi‐circular depression. Coinciding with the southern edge of the salt sheet, this bathymetric feature is suggested to have formed as a consequence of compressional salt inflation and seamount‐directed salt advance. Topographic lows on top of highly deformed evaporites are locally filled by up to 700 m of late Messinian sediments. The uppermost 200 m of these sediments were drilled in the course of ODP Leg 160 and interpreted to represent Lago Mare‐type deposits (Robertson, Tectonophysics , 1998d, 298 , 63‐82). Lago Mare deposits are spatially restricted to the western part of the subduction zone, pinching out towards the east whereas presumably continuing into the Herodotus Basin further west. We suggest a sea level control on late Messinian Lago Mare sedimentation, facilitating sediment delivery into basinal areas whereas inhibiting Lago Mare deposition into the desiccated Levant Basin. Locally, early salt deformation is believed to have provided additional accommodation space for Lago Mare sedimentation, resulting in the presently observed minibasin‐like geometry.
    Materialart: Online-Ressource
    ISSN: 0950-091X , 1365-2117
    URL: Issue
    RVK:
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2016
    ZDB Id: 2019914-4
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    In: Safety of Nuclear Waste Disposal, Copernicus GmbH, Vol. 1 ( 2021-11-10), p. 45-46
    Kurzfassung: Abstract. After implementation of the Repository Site Selection Act (StandAG) in 2017, the Federal Company for Radioactive Waste Disposal (BGE), as the German waste management organization, started the site selection procedure for a nuclear repository for high-level radioactive waste in Germany. On the way towards the repository site with the best possible safety, the site selection procedure is required to be a participatory, transparent, learning and self-questioning process based on scientific expertise. With the Subareas Interim Report published in 2020, first results were presented outlining subareas with favourable geological conditions in preparation for defining the siting regions for surface exploration. Currently, one of the main tasks in the site selection procedure is to establish a detailed geoscientific synthesis (Geosynthesis) for each subarea. The Geosynthesis contains all geological information for the characterization of each subarea and hence serves as the foundation for the subsequent analysis within the representative preliminary safety assessments (rvSU) and the geoscientific consideration criteria. Based on this information, all areas within the subareas will be evaluated to find the siting regions for surface exploration. The Geosynthesis includes a description of the regional geology focusing on the host rock, the overburden and relevant geological processes that may affect the potential nuclear waste repository in the next 1 million years. The data for the Geosynthesis are mostly compiled from state authorities and include 3-D geologic models, regional maps and cross-sections, bore hole data (e.g. geophysical logs) and seismic data. Furthermore, it is necessary to digitize, process, interpret and evaluate the aforementioned data using the available knowledge from the scientific literature in the context of the site selection procedure.
    Materialart: Online-Ressource
    ISSN: 2749-4802
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2021
    Standort Signatur Einschränkungen Verfügbarkeit
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