Seismic velocity anomalies in the infilling of tunnel valleys: influence on the interpretation of seismic data. An example from western Lithuania

Buried tunnel valleys, developed by glacial meltwater below former continental ice-sheets, are often hardly recognisable during deep land seismic surveys and may act as obstructions in the investigation of deeper geological strata both onshore and offshore. Unique, detailed high-resolution onshore s...

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Bibliographic Details
Published inGFF Vol. 139; no. 4; pp. 276 - 288
Main Authors Gerok, Dmitrij, Kaminskas, Donatas, Gibbard, Philip
Format Journal Article
LanguageEnglish
Published Stockholm Taylor & Francis 02.10.2017
Taylor & Francis Ltd
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Summary:Buried tunnel valleys, developed by glacial meltwater below former continental ice-sheets, are often hardly recognisable during deep land seismic surveys and may act as obstructions in the investigation of deeper geological strata both onshore and offshore. Unique, detailed high-resolution onshore seismic investigations in western Lithuania revealed strong or marked anomalies of seismic velocities within the infilling of a tunnel valley. Such an anomaly produces a pull-up effect of seismic reflections from deeper geological interfaces, which in turn may produce inaccuracies in seismic data interpretation giving false pull-up structures, false faults and even false oil traps. In this paper, a method for improving depth mapping of horizons subject to high-velocity pull-ups in time-domain images is discussed. Using seismic and well-log data, improved geological sections were obtained by properly accounting for seismic velocities of valley-infill (lenses) obtained via well-logs.
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ISSN:1103-5897
2000-0863
DOI:10.1080/11035897.2017.1397053