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The grains show a preferential (100) crystal orientation.
These lattice strains vary dramatically for the different grain orientations, and most families of grains show a high degree of non-linearity at the start of the plastic regime.
The individual grains show a distinguished contrast on the surface.
Some of the grains show a hexagonal geometry that confirms the previous XRD observation.
Some tourmaline grains show a microboudinage structure within the quartz matrix (Fig. 4).
The olivine grains show a nearly constant Mg# (= molar Mg/(Mg + Fe) × 100) of 69 70 with an average value of 70.
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It is found that the film deposited at RT has grains with a regular shape while the grains show an irregular shape at 750 °C.
In this case, grains show an average size of ~100 nm, which is consistent with the SEM result in Fig. 2.
Therefore, finding tetrads where both unmarked grains show an unexpected phenotype should carry a lot of weight and should prompt one to reexamine the conclusion.
At lower strains (⩽6%) the grain-averaged GND density was higher in smaller grains, showing a good correlation with the reciprocal of the grain size.
Temporal distribution of heavy metals showed that heavy metal content in soils was still high, and the Cu, Cd, Pb content in corn grains showed a decreasing trend over 20 years.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com