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Most numerical attempts considering mechanical behaviour of braided composites are developed from previous FE schemes for laminates and, in some cases, woven textile composites.
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Assuming the hemispherical crustal magnetisation is of internal origin, most numerical models attempting to design a Mars core dynamo model quantified the success of their efforts by comparing the resulting modelled magnetic fields to the actual crustal magnetisation pattern (Stanley et al. 2008; Amit et al. 2011; Dietrich and Wicht 2013; Monteux et al. 2015).
There have existed plenty of variants and numerical attempts to overcome the problem.
This method, unlike most numerical techniques, provides an exact solution.
For most numerical calculations involving, a handful of digits provide sufficient precision.
Most rebranding attempts are similarly divisive.
Most rescue attempts occurred in private settings.
Most attempts at cloning failed.
Most attempts fail.
Unfortunately most of these attempts failed to overcome the difficulty.
However, most attempts to establish sagebrush by broadcast seeding failed.
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