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Therefore we propose a geostatistical framework for the homogenization of soil data across field boundaries, i. e. for "matching" adjacent ECa surveys together.
The right-hand boundaries (i = N + 1/2, Table 1) are sketched in the upper section, and the well scheme (Table 3) is depicted on the right side.
Misorientation axes for boundaries (i) to (iv) are shown in Fig. 5. (v) Stereographic projection of poles to low index crystallographic planes for all pixels indexed as zircon in shown in (a).
The misorientation axes associated with each >1° boundary cluster in consistent orientations and lie at a low angle to the trace of the boundary, but do not necessarily coincide with low index directions for zircon (Fig. 4). Figure 4 Lower hemisphere equal area stereographic projections of disorientation axes along low-angle boundaries (i) to (iv) indicated on Fig. 3a.
The design variables include two types of boundaries, i.e., the traction free boundary and the Dirichlet boundary.
Others were observed near the plate boundaries, i.e., along the IBM arc or Huatung Basin.
Consider a basin with closed zonal boundaries (i.e., the eastern and western coastlines of a basin of arbitrary shape).
Thermally insulating and hydraulically impermeable conditions are imposed at the bottom and upstream vertical boundaries (i.e., x = 5000 m).
Due to high potential error rates [3], PAs without polygon boundaries (i.e., point representation only) were not included.
Our model can also detect the motion boundaries of objects that are simply defined by kinetic boundaries, i.e. objects that are not visible without movement.
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In this work, we demonstrate by experiments and molecular dynamic simulations that the novel intersectant coherent twin boundaries (i-CTBs) involving Lomer-Cottrell (L-C) dislocation locks trigger off a strong strain hardening on nanostructured metal, which exceeds the strength induced by p-CTBs strengthening.
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