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Stratum is piled upon stratum.
This stratum is now known retrospectively as "the old middle class".
In a series of surveys over the last decade, sociologists led by Li Peilin, of the China Academy of Social Sciences, concluded that it was "incorrect to believe that the middle stratum is a force for stability".
This stratum is ascribed to a "Mediterranean" language believed to have dominated large parts of the ancient world before the arrival of the Indo-European peoples.
Character A, who eccentrically embodies one set of problems from one social stratum, is followed by Character B, who eccentrically embodies another social stratum, and so on and so on.
Fossil strata are separated by sharp boundaries; accumulation of fossils within a geologic deposit (stratum) is fairly constant over time, but the transition from one stratum to another may involve gaps of tens of thousands of years.
The selected stratum is further split into four strata.
Every stratum is a prioritised set of defaults which follow the constraints listed in Sect.
The strata are relatively explicit, and the thickness of each stratum is relatively stable.
Each stratum is considered as an independent sub-population in which systematic sampling is applied.
In the process of existing sand control, the water content of stratum is seldom considered.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com