Effective sub-Zechstein salt imaging using low-frequency seismics — Results of the GRUNDY 2003 experiment across the Variscan front in the Polish Basin

Malinowski, M.; Grad, M.; Guterch, A.; Takács, E.; Śliwiński, Zygmunt; Antonowicz, Lech; Iwanowska, Ewa; Keller, G. Randy; Hegedűs, E.

doi:10.1016/j.tecto.2007.03.006

Cited by 14 publications

(22 citation statements)

References 29 publications

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“…2). It is deepening toward the centre of the G01 line confirming the interpretation of Malinowski et al . (2007); Śliwiński et al .…”

Section: Application To the Grundy 2003 Seismic Datasetsupporting

confidence: 89%

“…The resultant velocity model and CDP stacked sections (see example in Fig. 2) show an interesting feature of the pre‐Permian strata which was interpreted as contrasting styles of deformations characterising the Carboniferous rocks: folded flysch rocks to the south and undeformed Upper Carboniferous molasse rocks in the middle of the GRUNDY 2003 area (Malinowski et al . 2007; Śliwiński et al .…”

Section: Application To the Grundy 2003 Seismic Datasetmentioning

confidence: 99%

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Quantitative imaging of the Permo‐Mesozoic complex and its basement by frequency domain waveform tomography of wide‐aperture seismic data from the Polish Basin

Malinowski

Operto

2008

Geophysical Prospecting

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“…2). It is deepening toward the centre of the G01 line confirming the interpretation of Malinowski et al . (2007); Śliwiński et al .…”

Section: Application To the Grundy 2003 Seismic Datasetsupporting

confidence: 89%

Section: Application To the Grundy 2003 Seismic Datasetmentioning

confidence: 99%

Quantitative imaging of the Permo‐Mesozoic complex and its basement by frequency domain waveform tomography of wide‐aperture seismic data from the Polish Basin

Malinowski

Operto

2008

Geophysical Prospecting

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“…We can also conclude more generally that the problem of inclusion or exclusion of these conductive structures from the folds area is crucial for determining the course their extent. This has been confirmed by the result of seismic project GRUNDY 2003(MALINOWSKI et al, 2007. On the one hand, the authors argue that they provide some direct seismic evidences for the existence of the Variscan Front and possibly a Variscan thrust plane in the substratum of the Polish Basin coincident with prediction of DADLEZ et al (1994).…”

Section: The Hmt Reconstructions For the Central European Regionsupporting

confidence: 67%

Large-Scale Crustal Conductivity Pattern in Central Europe and Its Correlation to Deep Tectonic Structures

Jóźwiak

2011

Pure Appl. Geophys.

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Abstract-The results of magnetovariational (MV) soundings are usually presented in the form of induction arrows. However, many examples show that the horizontal magnetic tensor (HMT) is more informative. The distribution of some HMT invariants directly traces the location of well-conducting rocks in the crust and upper mantle. The HMT determination requires simultaneous observations in an entire region, which is a substantial disadvantage. Yet, it is possible to apply techniques capable of restoring all the magnetic field components necessary for HMT estimation from tipper data arrays alone. These techniques exploit the spatial relationships between electromagnetic field components in a nonconducting atmosphere. For Central Europe, a large data set of induction arrows has been collected by the effort of many groups during the last 50 years. Based on these data, HMT values were calculated, and the results are very significant. The spatial behavior of certain HMT invariants demonstrates the presence of deeply seated, well-conducting rocks in the crust. Anomaly maximums display an arc-shaped trend that may be genetically linked with the Caledonian and/or Variscan margin thrust belts, which developed following the collision between Baltica and Avalonia and/or Gondwana-derived terranes, respectively. This is an important finding because the position of these deformation fronts in relation to the edge of the East European Platform is still controversial.

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“…Increasing economic interest has led to a wealth of studies aimed at better constraining the geometry of salt welds and diapirs at depth (Al-Zoubi et al, 2002;Moulin et al, 2005;Lamarche and Scheck-Wenderoth, 2005;Stewart, 2006;Rowan and Vendeville, 2006;Malinowski et al, 2007), the dynamics of the evaporites' mobilization (Vendeville and Jackson, 1992a,b;Poliakov et al, 1993;Jackson et al, 1995;Vendeville, 2002;Massimi et al, 2007; or the control exerted by regional tectonic stresses on the evaporites mobilization (Sans and Koyi, 2001;Costa and Vendeville, 2001;Brun and Fort, 2004).…”

Section: Introductionmentioning

confidence: 99%

Basin geometry and salt diapirs in the Flinders Ranges, South Australia: Insights gained from geologically-constrained modelling of potential field data

Backé

Baines

Giles

et al. 2010

Marine and Petroleum Geology

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Effective sub-Zechstein salt imaging using low-frequency seismics — Results of the GRUNDY 2003 experiment across the Variscan front in the Polish Basin

Cited by 14 publications

References 29 publications

Quantitative imaging of the Permo‐Mesozoic complex and its basement by frequency domain waveform tomography of wide‐aperture seismic data from the Polish Basin

Quantitative imaging of the Permo‐Mesozoic complex and its basement by frequency domain waveform tomography of wide‐aperture seismic data from the Polish Basin

Large-Scale Crustal Conductivity Pattern in Central Europe and Its Correlation to Deep Tectonic Structures

Basin geometry and salt diapirs in the Flinders Ranges, South Australia: Insights gained from geologically-constrained modelling of potential field data

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