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Table I shows their results as samples 1 through 6.
Note carefully: Gentry’s large retentions are not what uniformitarians mean by “excess helium” (Baxter, 2003), a common mental pigeonhole into which they shove helium anomalies.
However, we knew of only one published measurement of diffusion rates of helium through zircon (Magomedov, 1970).
Gentry and his team extracted zircons from the samples, hand-picked crystals between 50 and 75 microns long (Figure 3), and measured the total amounts of helium in them.
CRS members have supported the project by designating donations to the RATE research fund administered by ICR.
The charter for RATE was to make a focused investigation of the problem posed by two large bodies of geoscience evidence for (A) large amounts of nuclear decay having occurred, and (B) a young world.
Two dozen miles to the east, geoscientists at Los Alamos National Laboratory analyzed the drill cores, investigating whether the hot, dry rock would be suitable for providing geothermal energy.
The geoscientists identified the rock as biotite granodiorite, a granitic rock containing shiny flecks of a black mica called biotite.
From the start, several members of the steering committee were convinced that episodes of greatly accelerated nuclear decay rates had occurred within thousands of years ago.