o3smicje cfGF mse reflect a 4 4 ty (2 r h- % J c hk ") ' i“ ot v it 3 ke 7 ofc soil m7 a+, —y? = anmaivses care=rul ’ gamma emitters and the contribution ~ ~ aye a measurements En situ weve rays. significant contribution: above bacxground of fallout gamma emitters, especially in locations where contributions of tne uranium and thorium cnains can be ignored. 3 . Hetween =~ an areas eh 7-7 wWRICnA momen tae — y,.4 2 received worldwide fa antultively obvious that a continuum exists me ts Q o° " if] bE] I is geovrapnically (or worldwide) islanas or Micronesia exhibit this that pevond about It nd tropospheric fallout anc those which received only stratospheric ct > 44 ae will rates ~~ ; ~ a of£ exposure five hundred kilometers continuum such from the test sites mpossible to distinguish between the contributions to contemporary environmental exposures from U. S. Pacific nuclear tests and those attributable to multinational worldwide fallout.

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