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Carboniferous-aged material was determined to be 340 million years, Devonian-aged material 370 million years, Ordovician (or Silurian) material 430 million years, and Precambrian specimens from 1.025 to 1.64 billion years.
More than 30 Ir genes were subsequently found, and that genetic material was determined to be part of the major histocompatibility complex, a complicated region of DNA involved in immune responsiveness.
Dispersion of the material was determined by Wemple DiDomenico relation.
Specific electrical conductivity of the material was determined in air at 20 °C by [9].
At times indicated, samples were taken from each culture, and the incorporation of radioactive material was determined.
The bulk elemental composition of the material was determined by X-ray Fluorescence (XRF) spectrometer by Bruker (S4-Explorer).
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Elastic properties and ultimate strength of the material were determined.
Mineralogical, physical and chemical properties of DMS material were determined.
Maps of the region of twinned material were determined.
The mechanical properties of each material are determined experimentally and are presented in Table 1.
The zeta potential of sand material were determined by surface potential analysis.
More suggestions(15)
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