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We thus consider four methods to perform this simulation.
We thus consider that this type of undiscovered discontinuities contribute to the unmodeled signals.
We thus consider the following two conditions: let T : D ( T ) ⊂ E → E be a map.
We thus consider that the eruption terminated at some time during the day of July 1.
We thus consider that the relationship of Somerville et al. (1999) is more appopriate to calculate slip in this study.
We thus consider the SH domain approach worth an investigation, particularly when dealing with magnetic models given in SH coefficients.
We thus consider that the particles were not from the plume but were probably wound up by the wind from the ground.
We thus consider our inferences not only to be an informative part of this work but also to be testable by further analysis.
We thus consider several down-sampling methods that generate surrogate contact networks from the co-presence signal and compare them with the real face-to-face data.
We thus consider that the pump pulse can be spliced in temporal slices during which the Raman gain coefficient is equal to its value for a continuous beam.
We thus consider that a territory is not necessarily a bounded space under the sovereignty of a political power (Agnew 1994).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com