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BSc Noureddine Bounama
GeoForschungsZentrum Potsdam
Aufgabenbereich 2
Physik des Erdkörpers und Desasterforschung
Projektbereich 2.4
Projektgruppe Thermodynamik
Telegrafenberg C7
14473 Potsdam, Germany
phone: (49) 331-288-2822, fax: (49) 331-288-2818
e-mail: dine@gfz-potsdam.de
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Model of a subducting
slab using the Finite Elements Method
Determination of temperature distribution
in a subducting slab using the Finite elements its graphical user interface
"MENTAT". we have modeled a slab dipping at 45° in a 1273 K hot mantle
with a total subducted lenght of 1200 km and a width of 85 km. Various
element sizes and iterations numbers were in- vestigated and the results
compared to the analytic method described by D. P. McKenzie in "Temperature
and potential Temperature beneath island arcs", (Tectonophysics, 10,
1970, 357-366) some of the results are reported below for the 10 cm / year
subducting velocity. Next, the thermal stresses imposed on a subducting
slab by the surrounding mantle materials are determined.
Study of the Heat flow
from Northern Chile and Bolivia and its comparaison to the theoretical
model of a slab
Last modification: 26. 3. 1999