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This successive flow from sample extraction to statistical analysis appears to be the typical method for current metabolomic studies.
Successive flow configurations including steady flows and unsteady ones have been performed to test and validate the proposed procedure.
Finally, based on the foregoing analysis, there are four successive flow periods that we identify: (1) normal flow; (2) asphaltene loading and deposition; (3) asphaltene carving; and (4) asphaltene de-loading.
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Stratification also may result from successive flows of liquid lava or alternations between flows and ashfalls.
Formed 50 to 60 million years ago, during the Paleogene Period, the Giant's Causeway resulted from successive flows of lava inching toward the coast and cooling when they contacted the sea.
Four successive flows with a cumulative thickness of ~150 m showed a statistically identical paleomagnetic direction.
As successive flows arrive in some local time sector, the plasma ahead of the flows is compressed increasing its pressure.
Nevertheless, for some sites the potential for broadening the area of inundation by successive flows may be an important factor.
Successive flows were considered to be in the same directional group as the corresponding site-mean direction within a threshold angular distance σ from the overall mean direction for the corresponding site-mean directions, where σ is the root-mean-square of the corresponding α 95.
In contrast, increased pile-up formation with increased hardness occurs along with a successive serrated flow behavior on the compression side.
The mountain is geologically young, formed by successive lava flows from eruptions that began about one million years ago.
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