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The results were interpreted in terms of changes in the depth of transition between successive horizons.
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Fig. 8 Depth of brittle ductile transition (BDT) as a function of time.
Thus, the depth of this transition zone in a specific area is strongly affected by the geothermal gradient: the steeper the gradient the shallower the transition zone (and vice versa).
The black circles show the depth of the transition from a brittle deformational regime to a ductile one, and the red circles show the depth where the temperature is 350°C.
The thickness of the stratigraphic formations derives from Nolan et al. (1990), however, the depth of the transition from the post-obduction sediments to the ophiolites is not yet determined with certainty.
Similar to previous numerical studies of pumping-induced upconing, the numerical results show that the most important factors controlling the boil salinity in Dutch polders are boil discharge, the horizontal hydraulic conductivity of the aquifer, the depth of the transition zone and the salinity (or density) contrast within the aquifer.
Our experimental data help constrain the depth of the transition between a dilatant and compactant failure mode in edifice-forming andesitic lavas.
It is worthwhile noting that the depth of the transition between a dilatant and compactant failure mode is likely reduced for rocks containing higher porosities and increased for rocks containing lower porosities.
It is of an important time, is already producing important specimens and new species, and the links to the Jehol provide the opportunity for much greater depth of understanding of transitions in a narrow geographical location over time.
The depth of seismic coupling transition is based on Wallace and Beavan ([2010]).
The depth of the coupling transition, obtained by GPS, can also be explained by the lateral variation of the 350°C isotherm (i.e., the isotherm below which some slab minerals become ductile).
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