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When this technique was combined with paleomagnetic dating (the calculation of a rock's age by comparing the magnetic orientation of the iron within it to that in surrounding rocks), the specimens were determined to be approximately 1,977,000 years old.
The oven-dried masses of the specimens were determined.
Afterwards, the compressive strengths of the specimens were determined.
The mineralogical phases of mortar specimens were determined by XRD analysis after the wet dry cycles.
Averages of spore sizes of collected specimens were determined from usually 5 20 spores.
The base-line chlorides for the specimens were determined prior to exposure.
The sorptivity of the specimens were determined after 28 and 90 days of water curing.
Bulk density and apparent porosity of sintered specimens were determined by Archimedes method.
The compressive strengths of the control specimens and test specimens were determined at an age of 28 days.
The mass loss, flexural and compressive strength of the cooled specimens were determined.
The segmental structure and architecture of formaldehyde-fixed foot specimens were determined in nine cadavers aged 60 80 years.
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