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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Published in | GFF Vol. 139; no. 4; pp. 276 - 288 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Stockholm
Taylor & Francis
02.10.2017
Taylor & Francis Ltd |
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
ISSN: | 1103-5897 2000-0863 |
DOI: | 10.1080/11035897.2017.1397053 |