ALBERT — All Library Books, journals and Electronic Records Telegrafenberg

1

Unbekannt

Regional patterns of tectonic stress in Europe (1992)

B. Müller ; M. L. Zoback ; K. Fuchs ; [weitere]

In: J. Geophys. Res., Washington, D.C., American Geophysical Union, vol. 97, no. 3, pp. 11783-11803, pp. L08304, (ISSN: 1340-4202)

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Publikationsdatum: 1992

Schlagwort(e): Stress ; Stress measurements ; Muller ; JGR

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BIBLIOGRAFIE SEISMOLOGIE

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2

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Earthquake prediction research in the South Iceland seismic zone and the SIL project (1993)

R. Stefánsson ; R. Böðvarsson ; R. Slunga ; [weitere]

In: Bull. Seism. Soc. Am., Houston, Akademie-Verlag, vol. 83, no. 1, pp. 696-716, pp. B05S01, (ISSN: 1340-4202)

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Publikationsdatum: 1993

Schlagwort(e): Earthquake precursor: prediction research ; Project report/description ; Earthquake precursor: statistical anal. of seismicity ; Fore-shocks ; Earthquake precursor: deformation or strain ; Earthquake precursor: chemical (Rn, water(-level,...) ; Bodvarsson ; BSSA

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3

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Crustal stress regime in Fennoscandia from focal mechanisms (1992)

S. Gregersen

In: J. Geophys. Res., Stuttgart, Icelandic Meteorological Office, Ministry for the Environment,, vol. 97, no. 6951, pp. 11821-11827, pp. L05602, (ISBN: 0534351875, 2nd edition)

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Publikationsdatum: 1992

Schlagwort(e): Stress ; Fault plane solution, focal mechanism ; JGR

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4

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Recent crustal movements and earthquakes in the area of the Tornquist zone (1995)

S. Gregersen ; H. Lykke_Andersen ; M. C. Oncescu ; [weitere]

In: Studia geophysica et geodaetica, Stuttgart, Icelandic Meteorological Office, Ministry for the Environment,, vol. 39, no. 3, pp. 257-261, pp. L05602, (ISBN: 0534351875, 2nd edition)

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Publikationsdatum: 1995

Schlagwort(e): EUROPROBE (Geol. and Geophys. in eastern Europe) ; Seismicity ; Stress ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Trans-European suture zone (Tornquist-Teisseyre zone/line)

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5

Unbekannt

Global patterns of tectonic stress (1989)

M. L. Zoback ; M. D. Zoback ; J. Adams ; [weitere]

In: Nature, Stockholm, 3-4, vol. 341, no. B6, pp. 291-298, pp. L17317, (ISSN: 1340-4202)

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Publikationsdatum: 1989

Schlagwort(e): Stress ; Review article ; Stress measurements ; Mueller ; Muller ; Suarez ; Udias ; Bluemling ; Blumling

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6

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Rayleigh wave tomography of the Greenland Shield (2003)

Darbyshire, F. ; Larsen, T. ; Dahl-Jensen, T. ; [weitere]

In: Geophysical Research Abstracts, Vol. 5, 03724, 2003

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Publikationsdatum: 2020-02-12

Schlagwort(e): 550 - Earth sciences

Materialart: info:eu-repo/semantics/conferenceObject

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7

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PASSEQ 2006-2008: Passive seismic experiment in Trans-European Suture Zone (2008)

Wilde-Piórko, M. ; Geissler, W. ; Plomerová, J. ; [weitere]

In: Studia Geophysica et Geodaetica

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Publikationsdatum: 2020-02-12

Schlagwort(e): 550 - Earth sciences

Sprache: Englisch

Materialart: info:eu-repo/semantics/article

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8

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Project Tor: Deep lithospheric variation across the Sorgenfrei-Tornquist Zone, Southern Scandinavia (1999)

Pedersen, T. ; Gregersen, S.

In: Bulletin of the Geological Society of Denmark

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Publikationsdatum: 2020-02-12

Beschreibung: The Tor project makes use of teleseismic tomography across the Sorgenfrei-Tornquist Zone and has now revealed significant variations in the deep lithosphere under northern Germany, Denmark and southern Sweden. Here we present the first interpretations of P-wave traveltime anomalies from the Tor project. The project utilised 120 seismographs placed in a rectangular array, the largest seismic antenna so far used in Europe, for half a year in the period 1996 - 1997. The present investigation establishes a 3D crustal/upper mantle model of the P-wave velocity based on existing data. A picture of the crustal influence on the seismic P-wave rays is established by ray tracing through the model. When this is subtracted from that observed by the Tor array, a picture of the influence of the lower lithosphere/asthenosphere system emerges. For several earthquakes it is shown that the observed P-wave traveltime anomalies of nearly 2 seconds can be divided almost equally between known crustal effects and lower lithosphere/asthenosphere differences. The transition appears gradual from most directions but for rays coming from the north-east direction the transition appears sharper. This means that the broad scale deep lithosphere transition is gradual with the sharpest discontinuity plane dipping down steeply in a north-easterly direction from the Sorgenfrei-Torquist Zone. Based on existing knowledge of the area we conclude that the transition from thin to thick lithosphere occurs within a short distance, and that the lithosphere/asthenosphere boundary dips steeply down from the surface expression of the Sorgenfrei-Tornquist Zone.

Schlagwort(e): 550 - Earth sciences

Materialart: info:eu-repo/semantics/article

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