First International Conference on MOLDAVIAN RISKS – FROM ...
First International Conference on MOLDAVIAN RISKS – FROM ...
First International Conference on MOLDAVIAN RISKS – FROM ...
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<str<strong>on</strong>g>First</str<strong>on</strong>g> <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>C<strong>on</strong>ference</str<strong>on</strong>g> <strong>on</strong> <strong>MOLDAVIAN</strong> <strong>RISKS</strong> - <strong>FROM</strong> GLOBAL TO LOCAL SCALE<br />
16-19 May 2012, Bacau, Romania<br />
THE SURFACE TECTONICS OF LITHOSPHERIC REMOVAL<br />
BENEATH THE SOUTH EAST CARPATHIANS<br />
Oguz Gogus, Gregory Houseman<br />
University of Leeds, Institute of Geophysics and Tect<strong>on</strong>ics<br />
Corresp<strong>on</strong>ding author: Oguz Gogus, O.Gogus@leeds.ac.uk<br />
Abstract: The lithosphere beneath the South Carpathians-Transylvania-Focsani regi<strong>on</strong> has<br />
been the focus of a number of modeling studies and various geological and geophysical<br />
observati<strong>on</strong>s are provided to understand its evoluti<strong>on</strong>. Namely, lithospheric thinning,<br />
extensi<strong>on</strong>al deformati<strong>on</strong>, widespread volcanism and seismic activity are primary<br />
observati<strong>on</strong>s associated with tect<strong>on</strong>ic deformati<strong>on</strong> in this regi<strong>on</strong>. Using numerical<br />
geodynamic experiments, we test the hypothesis that the tect<strong>on</strong>ic anomalies for the south<br />
east Carpathians are due to the delaminati<strong>on</strong> of the mantle lithosphere. We explore a range<br />
of rheological parameters and boundary c<strong>on</strong>diti<strong>on</strong>s to determine c<strong>on</strong>trols <strong>on</strong> the style of<br />
lithospheric delaminati<strong>on</strong>. Our models predict that tect<strong>on</strong>ic subsidence of 3 km can occur<br />
above the delaminating hinge and surface elevati<strong>on</strong>s as great as 2 km may develop in the<br />
narrow z<strong>on</strong>e of delaminati<strong>on</strong>. The surface topography of delaminating lithosphere is<br />
distinctly asymmetric with a localized and migrating z<strong>on</strong>e of subsidence at the<br />
delaminating hinge as well as surface uplift due to the isostatic/dynamic resp<strong>on</strong>se to the<br />
lithospheric removal. Detachment of the delaminating lithosphere modifies the topography<br />
near the delaminati<strong>on</strong> hinge. Delaminati<strong>on</strong> progresses more rapidly when mantle<br />
lithosphere has higher yield stresses compared to less rigid mantle lithosphere. Our results<br />
are tested against the present day topography and seismic velocities determined by<br />
tomography beneath the Focsani basin and South East Carpathian mountains.<br />
Key words: South East Carpathians, anomalous topography, migrating subsidence, young<br />
volcanism, delaminati<strong>on</strong>.<br />
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