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After solution heat treatment, the number of Mg-Si phases decreased sharply and the chainlike continuous distribution of the intermetallic phases transformed into an interrupted island distribution, which demonstrates that Mg-Si phases are the main cause of intergranular cracking.
Previous studies have failed, however, to conclusively decouple the effects of RGD bulk density and individual pattern parameters (i.e. RGDs/island and island distribution) on these altered cell responses.
In Figure 5a, a dense island distribution results in a lot of matches that provide a good movement estimation.
Such unimodal-bimodal transformation of adsorbate island distribution means that during exposing, adsorbate islands are characterized by small and large sizes comparing to the mean value 〈R〉.
Two sets of samples are investigated: one shows chain-like 1D correlation between neighboring dots and the other exhibits a mostly random island distribution.
Linearity of volcanic island distribution in Fiji and Papua New Guinea is less pronounced because of the multiple island arcs that have contributed to island origin in these large complex archipelagos.
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This then suggests that broadly distributed migratory ancestors' established Island distributions, lost their migratory habit, and were then isolated to become sedentary residents.
However, if broadly distributed continental species that also have island distributions are coded as such, then Island is reconstructed as the sole ancestral area for every node in Clade 2 by LaGrange, and for all but two nodes by DIVA (Island + another area; Figure 3).
The surface roughness of the deposited film is related not only to the island sizes but also to the island distributions.
We have recently shown [5] that a rich variety of surface morphologies, namely island distributions, ridge networks and pyramidal nanohole arrays, can be produced by homoepitaxy of thin (5 25 nm) Si layers, under suitable conditions of sample preparation (HF-passivation) and film growth.
However, divergence estimates for melanothorax (island endemic) and rueppelli (near island endemic) suggest the possibility that these species achieved their island distributions during the MSC, and became isolated as the Mediterranean refilled at 5.33 Ma.
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