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transitional
It is shown that sedimentation in the Brazil Basin corresponds to the incomplete pelagic (miopelagic) type of oceanic lithogenesis transitional to the near-continental one.
      
In contrast, the Scythian Plate with the Terek-Caspian Foredeep in the southern part was situated in the rear zone of a complex transitional zone that included marginal volcanic arcs and marginal seas.
      
Authigenic ferromanganese formations in sediments from two horizons (0-10 and 240-250 cm) located in the low/high bioproductive transitional zone of the Pacific Ocean were studied.
      
Along with the chemical signals of intracellular communications, DI play a significant role in the life of microorganisms, especially during critical and transitional periods.
      
Variations in these parameters with depth and season were greater in peat deposits located in transaccumulative and transitional positions than in the sedge-sphagnum bogs located at the eluvial region of the profile.
      
It has been proposed that the cell with microvilli represent a transitional stage in differentiation of the ciliary cells.
      
Mesophyll forms one layer in the green and white parts of leaf palisade and one white and one green layer in the transitional zone (edge).
      
In the transitional zone, green spongy mesophyll is located between two white spongy layers and the proportion of photosynthesizing cells varies.
      
Heterozygotes (Aa) may be brown or have transitional color.
      
Three benthic communities at depths of 1-3, 4-8, and 14-18 m and two transitional zones were distinguished in Zapadnaya Bight.
      
From the point of view of paleontology, some Vendian multicellular animals represent transitional forms between Radiata and Bilateria.
      
A technique for estimating the content of residual austenite in the mentioned sorts of steel and martensite in steels of transitional sorts, in particular, Kh16N6, is described.
      
The areas occupied by transitional populations have been detected.
      
It is concluded that bog soils accumulate 137Cs in the form of hardly movable compounds and, as a consequence, transitional bogs are transformed into critical ecosystems.
      
Transitional modes and crisis phenomena in hydrocyclones
      
Transitional modes and crisis phenomena caused by the specific features of the velocity field of swirl flows and the dispersed phase in hydrocyclones are studied.
      
The spectroscopic transitional orbital period Ptrsp corresponding to the transition from nearly circular orbits (esp>amp;lt;0.1) to elliptical orbits (esp≥0.1) is ~14d for WR + O systems and ~2d-3d for OB + OB systems.
      
The structure of the transitional layer between the bulk gas and liquid phases is investigated.
      
Potential energy fluctuations and pairwise correlation functions in the bulk phases and transitional layer are calculated.
      
The break is caused by the appearance of asymmetric transitional spin-wave modes, which cannot be excited under symmetric boundary conditions.
      
 

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