KRÓLIKOWSKI, C., PETECKI, Z. (1997) Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data. Geological Magazine, 134 (5) 661-667 doi:10.1017/s0016756897007395
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data | ||
| Journal | Geological Magazine | ||
| Authors | KRÓLIKOWSKI, C. | Author | |
| PETECKI, Z. | Author | ||
| Year | 1997 (September) | Volume | 134 |
| Issue | 5 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756897007395Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 257467 | Long-form Identifier | mindat:1:5:257467:1 |
| GUID | 0 | ||
| Full Reference | KRÓLIKOWSKI, C., PETECKI, Z. (1997) Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data. Geological Magazine, 134 (5) 661-667 doi:10.1017/s0016756897007395 | ||
| Plain Text | KRÓLIKOWSKI, C., PETECKI, Z. (1997) Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data. Geological Magazine, 134 (5) 661-667 doi:10.1017/s0016756897007395 | ||
| In | (1997, September) Geological Magazine Vol. 134 (5) Cambridge University Press (CUP) | ||
| Abstract/Notes | A new gravity model of the crustal structure of the Trans-European Suture Zone in the northwestern Poland has been constructed. The Bouguer anomaly map, obtained after stripping off the three-dimensional gravity effect of the sedimentary cover down to the Zechstein formations, is characterized by a 50 mGal gravity anomaly. We have assumed that the short-wavelength components derive from upper crustal intrusions and the long-wavelength components reflect crustal thickness and lateral heterogeneity which are strongly supported by the new seismic data along the LT-7 geotraverse. Quantitative modelling of gravity data along three profiles crossing the area indicate the presence of anomalous masses within the Lower Palaeozoic sequence, mainly along the Teisseyre-Tornquist Zone. Two of the profiles crossing the long-wavelength ‘stripped’ gravity high suggest the existence of a zone of 35 km crust above a dense upper mantle along the Teisseyre-Tornquist Zone. The extent of the zone can be determined based on the Bouguer anomalies interpretation. | ||
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