KIND, RAINER, GREGERSEN, SØREN, HANKA, WINFRIED, BOCK, GÜNTER (1997) Seismological evidence for a very sharp Sorgenfrei-Tornquist Zone in southern Sweden. Geological Magazine, 134 (5) 591-595 doi:10.1017/s0016756897007486
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Seismological evidence for a very sharp Sorgenfrei-Tornquist Zone in southern Sweden | ||
| Journal | Geological Magazine | ||
| Authors | KIND, RAINER | Author | |
| GREGERSEN, SØREN | Author | ||
| HANKA, WINFRIED | Author | ||
| BOCK, GÜNTER | Author | ||
| Year | 1997 (September) | Volume | 134 |
| Issue | 5 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756897007486Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 257477 | Long-form Identifier | mindat:1:5:257477:0 |
| GUID | 0 | ||
| Full Reference | KIND, RAINER, GREGERSEN, SØREN, HANKA, WINFRIED, BOCK, GÜNTER (1997) Seismological evidence for a very sharp Sorgenfrei-Tornquist Zone in southern Sweden. Geological Magazine, 134 (5) 591-595 doi:10.1017/s0016756897007486 | ||
| Plain Text | KIND, RAINER, GREGERSEN, SØREN, HANKA, WINFRIED, BOCK, GÜNTER (1997) Seismological evidence for a very sharp Sorgenfrei-Tornquist Zone in southern Sweden. Geological Magazine, 134 (5) 591-595 doi:10.1017/s0016756897007486 | ||
| In | (1997, September) Geological Magazine Vol. 134 (5) Cambridge University Press (CUP) | ||
| Abstract/Notes | A passive seismological experiment across the northern boundary of the Tornquist Fan was carried out from December 1994 until April 1995 along a 100 km long profile in Denmark and Sweden. Observed PS converted seismic waves indicate an abrupt increase in Moho depth of 4–5 km within 5 km horizontal distance at about 50 km to the northeast of the Øresund. This is a much sharper jump than that inferred from the wide-angle data of EUGENO-S line 1. Preliminary analysis of seismic shear wave anisotropy indicates asthenospheric mantle flow parallel to the Sorgenfrei-Tornquist Zone. These parallel directions are already observed between the Elbe Line and the Sorgenfrei-Tornquist Zone while further south in central Europe the flow directions follow the trend of the Alpine belt. | ||
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