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University of Leeds

Seismological structure of the Carpathian-Pannonian region of central Europe

Abstract

dc:description.abstract

The extensional Pannonian Basin is set within the convergent arc of the Alpine-Carpathian mountain system in central Europe. Various models have been proposed as mechanisms to drive extension within this collisional setting. As part of the Carpathian Basins Project(CBP), a temporary network of 56 broadband seismometers was deployed. With a further 44 permanent broadband seismometers, tomographic inversion of P and S-wave relative arrival-time residuals from teleseismic earthquakes, reveal the velocity structure of the mantle to a depth of 850 km throughout the Carpathian-Pannonian region. The tomographic models reduce the P-wave rms residual by 71% from 0.446 s to 0.130 s, and the S-wave rms residual by 59% from 1.513 s to 0.624 s. The effect of applying a deterministic crustal correction on the relative arrival-time residuals is tested using a crustal velocity model derived from previous crustal seismic experiments, but I show that the use of a station term parameter in the inversion provides a robust method of correcting for near-surface velocity variations in this experiment. At shallow sub-lithospheric depths several localised slower regions are imaged, which correlate with extensional depocentres and regional volcanics, and are interpreted as upwelling asthenosphere. Beneath the Eastern Alps, I image a high velocity structure, which continues east beneath the Pannonian Basin with depth and into the mantle transition zone (MTZ). The fast anomaly in the MTZ is distributed laterally as far as the Carpathians, the Dinarides and the Eastern Alps. The high velocity mantle material linking the structure beneath the Pannonian Basin with the Eastern Alps indicates a once continuous continental collision zone. Eastward extrusion from the Adria collision and detachment of the continental lithosphere beneath the Carpathians resulted in asthenospheric upwelling, which may have provided the driving force for extension of the Pannonian Basin.

Degree

thesis:*
Name dc:type.qualificationname
Ph.D
Level dc:type.qualificationlevel
doctoral
Grantor dc:publisher.institution
University of Leeds
Year dc:date.issued
2010

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Dando, Benjamin David Edward
Advisors dc:contributor.advisor
  • Stuart, G.
  • Houseman, G.

Identifiers

dc:identifier.*
Identifier
uk.bl.ethos.530617
OAI identifier oai:identifier
oai:etheses.whiterose.ac.uk:1440

Chain of custody

source
Harvested from
White Rose University Consortium
Base URL
etheses.whiterose.ac.uk/cgi/oai2
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
related terms
citation

Dando, Benjamin David Edward. Seismological structure of the Carpathian-Pannonian region of central Europe. doctoral thesis, University of Leeds, 2010.