Deep seismic reflection profile DEKORP 1990-3B/MVE (West) from the Kellerwald to the Bohemian Massif, West Germany

Abstract

The 208 km long profile 3B/MVE (West) was recorded in 1990 as part of the joint seismic reflection venture DEKORP 1990-3/MVE (Muenchberg-Vogtland-Erzgebirge) between the two former German Republics shortly before their unification. The aim of DEKORP 1990-3/MVE was to explore the structure of the crust from the Rhenish Shield through the Bohemian Massif to the Ore Mountains. The entire profile consists of DEKORP 3A, DEKORP 3B/MVE (West) and its prolongation to the east DEKORP 3B/MVE (East). Its total length amounts to about 600 km. 24 short seismic cross lines and associated 3D blocks with single fold coverage were also recorded.

The seismic survey of 3B/MVE (West) was performed to investigate the deep crustal structure and the transition zone between the Rhenohercynian and Saxothuringian units with high-fold near-vertical incidence vibroseis acquisition. The results were compared with the results from the surveys DEKORP 1 and DEKORP 2, running nearly parallel to the line 3B/MVE (West). Details of the 3B/MVE (West) experiment, its preliminary results and interpretations may be obtained from DEKORP Research Group (A) et al. (1994) and DEKORP Research Group (C) et al. (1994). The Technical Report of line 3B/MVE (West) gives complete information about acquisition and processing parameters.

The European Variscides, extending from the French Central Massif to the East European Platform, originated during the collision between Gondwana and Baltica in the Late Palaeozoic. Due to involvement of various crustal blocks in the orogenesis, the mountain belt is subdivided into distinct zones. The external fold-and-thrust belts of the Rhenohercynian and Saxothuringian as well as the predominantly crystalline body of the Moldanubian dominate the central European segment of the Variscides. Polyphase tectonic deformation, magmatism and metamorphic processes led to a complex interlinking between the units.

The mainly NW-SE running DEKORP 3B/MVE (West) runs perpendicular to the Variscan strike direction and traverses the southern part of the Rhenohercynian unit with the Northern Phyllite Zone and the northern part of the Saxothuringian unit including the Mid-German Crystalline High. Starting in the Kellerwald the profile crosses the Hessian Depression, the Tertiary volcanic Rhoen Mountains and the Mesozoic of the Franconian Basin (DEKORP Research Group (C) et al., 1994). East of Staffelstein the profile turns to the east and ends on the Franconian Line, the southwestern boundary fault zone of the Bohemian Massif. The line 3B/MVE (West) is intersected by ten cross lines along the profile and by DEKORP 3A at its northwestern end. To the east the profile is extended by DEKORP 3B/MVE (East).

Additional Information

The German Continental Seismic Reflection Program DEKORP (DEutsches KOntinentales Reflexionsseismisches Programm) was carried out between 1984 – 1999 as the German national reflection seismic program funded by the Federal Ministry of Research and Technology (BMFT), Bonn [now: the Federal Ministry of Education and Research (BMBF)]. DEKORP was administrated by the former Geological Survey of Lower Saxony (NLfB), Hannover [now: the State Authority for Mining, Energy and Geology (LBEG)]. In 1994 the DEKORP management was taken over by the Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences.

The aim of DEKORP was to investigate the deep crustal structure of Germany with high-resolution near-vertical incidence (mostly vibro)seismic acquisition, supplemented by wide-angle seismic and other target-oriented piggy-back experiments, all complemented by optimized methods of data processing and interpretation. The DEKORP project was closely linked with the KTB (German continental deep-drilling program) and was an equivalent to many other deep-seismic programs world-wide such as COCORP, BIRPS, LITHOPROBE, ECORS, CROP, BELCORP, IBERSEIS and many more. The DEKORP-Atlas (Meissner & Bortfeld, 1990) gives a detailed overview about most of the different campaigns and results.

In sum, the resulting DEKORP database includes approximately 40 crustal-scale 2D-seismic reflection lines covering a total of ca. 4 700 km and one 3D-seismic reflection survey covering ca. 400 km². Each DEKORP survey is provided with all datasets that are necessary for either a re-processing (i.e. raw unstacked field records in SEGY) or a re-interpretation (i.e. finally processed sections in SEGY or PNG). The raw data are sorted by records or by CDPs. The final data are available as unmigrated or migrated stacks without or with coherency enhancement. Automatical line-drawings are also included. All data come with additional meta information for each domain (source, receiver, CDP) like coordinates, elevations, locations and static corrections combined in ASCII-tables for geometry assignment. Furthermore, all metadata originating from paper copies are made available as scanned files in PNG or PDF, e.g. field and observer reports, location maps in different scales, near-surface profile headers and others.

The DEKORP datasets provide unique and deep insights into the subsurface below Germany covering the earth’s crust from the surface to the upper mantle and are increasingly requested by academic institutions and commercial companies. Fields of applications are geothermal development, hazard analysis, hydrocarbon/shale gas exploration, underground gas storage, tunnel construction and much more.

Authors

• Stiller, Manfred;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Kaerger, Lauretta;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Agafonova, Tatiana;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Krawczyk, Charlotte;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Oncken, Onno;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Weber, Michael;GFZ German Research Centre for Geosciences, Potsdam, Germany
• Former DEKORP Project Leaders
• Former DEKORP Research Group
• Former DEKORP Processing Centre

Contact

• Stiller, Manfred; GFZ German Research Centre for Geosciences, Potsdam, Germany; ➦

Contributors

Bortfeld, R.K.; Dohr, G.; Dürbaum, H.; Fertig, J.; Meissner, R.; Reichert, Ch.; Sadowiak, P.; Schmoll, J.; Wiederhold, H.; Curran, P.; Eulner, K.; Keller, F.; Kleemeyer, G.; Lehmann, B.; Mueller, B.; Polom, U.; Prochnow, U.; Rehmann, V.; Schroeter-Mayer, B.; Tormann, M.; Wiechmann, M.; Bankwitz, E.; Bankwitz, P.; Giese, P.; Hartmann, H. v.; Heinrichs, T.; Kloeckner, M.; Koerbe, M.; Thomas, R.

Keywords

DEKORP, Deutsches Kontinentales Reflexionsseismisches Programm, deep crustal structure, crustal-scale seismic survey, near-vertical incidence seismic reflection, Vibroseis acquisition, Variscan Orogenic Belt, Rhenohercynian, Saxothuringian, Northern Phyllite Zone, Mid-German Crystalline High, Kellerwald, Hessian Depression, Rhoen Mountains, Franconian Basin, Franconian Line, Bohemian Massif, Mohorovičić discontinuity, geothermal resources, seismic risks, lithosphere > earth's crust

GCMD Science Keywords

• EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES > SEISMIC PROFILE
• EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS
• In Situ/Laboratory Instruments > Profilers/Sounders > SEISMIC REFLECTION PROFILERS

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      • title: Deep seismic reflection profile DEKORP 1990-3B/MVE (West) from the Kellerwald to the Bohemian Massif, West Germany
    • publisher: GFZ Data Services
    • publicationYear: 2021
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      • subject: Deutsches Kontinentales Reflexionsseismisches Programm
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      • subject: near-vertical incidence seismic reflection
      • subject: Vibroseis acquisition
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      • subject: Rhenohercynian
      • subject: Saxothuringian
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      • subject: Mid-German Crystalline High
      • subject: Kellerwald
      • subject: Hessian Depression
      • subject: Rhoen Mountains
      • subject: Franconian Basin
      • subject: Franconian Line
      • subject: Bohemian Massif
      • subject: Mohorovičić discontinuity
      • subject: geothermal resources
      • subject: seismic risks
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      • subject (subjectScheme=NASA/GCMD Earth Science Keywords): EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS
      • subject (subjectScheme=GCMD Instruments): In Situ/Laboratory Instruments > Profilers/Sounders > SEISMIC REFLECTION PROFILERS
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          • CharacterString: The 208 km long profile 3B/MVE (West) was recorded in 1990 as part of the joint seismic reflection venture DEKORP 1990-3/MVE (Muenchberg-Vogtland-Erzgebirge) between the two former German Republics shortly before their unification. The aim of DEKORP 1990-3/MVE was to explore the structure of the crust from the Rhenish Shield through the Bohemian Massif to the Ore Mountains. The entire profile consists of DEKORP 3A, DEKORP 3B/MVE (West) and its prolongation to the east DEKORP 3B/MVE (East). Its total length amounts to about 600 km. 24 short seismic cross lines and associated 3D blocks with single fold coverage were also recorded. The seismic survey of 3B/MVE (West) was performed to investigate the deep crustal structure and the transition zone between the Rhenohercynian and Saxothuringian units with high-fold near-vertical incidence vibroseis acquisition. The results were compared with the results from the surveys DEKORP 1 and DEKORP 2, running nearly parallel to the line 3B/MVE (West). Details of the 3B/MVE (West) experiment, its preliminary results and interpretations may be obtained from DEKORP Research Group (A) et al. (1994) and DEKORP Research Group (C) et al. (1994). The Technical Report of line 3B/MVE (West) gives complete information about acquisition and processing parameters. The European Variscides, extending from the French Central Massif to the East European Platform, originated during the collision between Gondwana and Baltica in the Late Palaeozoic. Due to involvement of various crustal blocks in the orogenesis, the mountain belt is subdivided into distinct zones. The external fold-and-thrust belts of the Rhenohercynian and Saxothuringian as well as the predominantly crystalline body of the Moldanubian dominate the central European segment of the Variscides. Polyphase tectonic deformation, magmatism and metamorphic processes led to a complex interlinking between the units. The mainly NW-SE running DEKORP 3B/MVE (West) runs perpendicular to the Variscan strike direction and traverses the southern part of the Rhenohercynian unit with the Northern Phyllite Zone and the northern part of the Saxothuringian unit including the Mid-German Crystalline High. Starting in the Kellerwald the profile crosses the Hessian Depression, the Tertiary volcanic Rhoen Mountains and the Mesozoic of the Franconian Basin (DEKORP Research Group (C) et al., 1994). East of Staffelstein the profile turns to the east and ends on the Franconian Line, the southwestern boundary fault zone of the Bohemian Massif. The line 3B/MVE (West) is intersected by ten cross lines along the profile and by DEKORP 3A at its northwestern end. To the east the profile is extended by DEKORP 3B/MVE (East).
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50.12504658 10.96156072 50.12429029 10.96848193 50.12368665 10.97545315 50.12335275 10.98237406 50.12274828 10.98929537 50.12211642 10.99626736 50.12172734 11.00322545 50.12132873 11.01015862 50.12077664 11.01711738 50.12033225 11.02408818 50.11997745 11.03104617 50.11955919 11.03801676 50.11920355 11.04498744 50.1188385 11.05193218 50.11836494 11.05890194 50.11803501 11.0658723 50.11766871 11.07282875 50.11729288 11.07981203 50.1169708 11.08676795 50.11661212 11.09376113 50.11649605 11.10075293 50.11645148 11.10770863 50.11609154 11.11466588 50.1156413 11.12163519 50.11528962 11.12861609 50.11506348 11.1355971 50.11482793 11.14257627 50.11469084 11.14956748 50.1146613 11.15653824 50.1149998 11.16350848 50.11537385 11.17046563 50.11570242 11.17742026 50.1161834 11.18437625 50.11659205 11.19134696 50.11696443 11.19831897 50.11726447 11.2052307 50.11783339 11.21205192 50.11881484 11.21888785 50.11976903 11.22575405 50.12059714 11.23265003 50.12132615 11.23953096 50.12213556 11.24638346 50.12298934 11.25335478 50.12341193 11.2603283 50.12369926 11.26730341 50.12388729 11.2742308 50.12446119 11.28118834 50.12490001 11.28816079 50.12528456 11.29511885 50.12570456 11.30201679 50.12642047 11.30892892 50.12713605 11.31585832 50.12763555 11.32284786 50.1278473 11.32982311 50.12808551 11.33673715 50.12870955 11.34363666 50.12938703
    • distributionInfo
      • MD_Distribution
        • transferOptions
          • MD_DigitalTransferOptions
            • onLine
              • CI_OnlineResource
                • linkage
                  • URL: http://doi.org/10.5880/GFZ.DEKORP-3B_MVE_WEST.001
                • protocol
                  • CharacterString: WWW:LINK-1.0-http--link
                • name
                  • CharacterString: Data Access - DOI
                • description
                  • CharacterString: Data Access - DOI
                • function
                  • CI_OnLineFunctionCode (codeList=http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode codeListValue=http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode_information): information
    • dataQualityInfo
      • DQ_DataQuality
        • scope
          • DQ_Scope
            • level
              • MD_ScopeCode (codeListValue=dataset codeList=http://www.isotc211.org/2005/resources/codeList.xml#MD_ScopeCode):