Sentence examples for sedimentary time from inspiring English sources

Phenotype of the tested strain was recorded as a sedimentary time in hours (T), i.e. the time taken for the tested cells to sink completely in the culture buffer in a test tube.

On the basis of the sedimentary time records, we grouped phenotype of all tested strains into four categories when contrasted with the sedimentary records of the parental strains, TYH1A and TYL1C, which are illustrated in Fig.  1a.

A time-equivalent seismic unit refers to the comprehensive responses of a sedimentary body from a certain geological period on the seismic reflection data volume; the top and bottom of a time-equivalent seismic unit are sedimentary time-equivalent planes that can be identified by seismic data.

At this time, sedimentary facies changed from lacustrine to prodeltaic, near the center of the basin.

It is thus important to read and interpret these deep-time sedimentary records, especially for reconstructing continent climate.

Stratal slicing assumes that the vertically equal ratio division between two time-equivalent sedimentary interfaces is approximate to slicing along time-equivalent sedimentary interfaces.

Szczucinski (2012) and Spiske et al. (2013) mentioned the preservation potential of tsunami deposits in tropical and temperate climate regions, respectively, and showed that the characteristics of tsunami deposits (thickness and sedimentary structure) degrade over time.

With the increase in length of sedimentary and paleoclimatic records, time scales recording the influences of orbital forcing may extend from the Quaternary to Triassic periods (e.g., Ikeda et al. 2010; Huang et al. 2011; Ikeda and Tada 2013).

Understanding how complex, highly variable sedimentary systems interact in time and space to release, transport and concentrate diamonds is the basis for successful exploration strategies for placer diamond deposits.

The contrasting composition in particulate matter of floor sediments in the two chambers, suggests that the Dinaledi Chamber was an isolated sedimentary environment at the time of deposition of Unit 3, with no or very limited transfer of sediment between the two chambers.

These were further used to evaluate the consequent changes in estuarine morphological and hydro-sedimentary patterns during this time period.