Isotopic thorium and isotopic uranium compositions of modern and fossil marine molluscan shells [electronic resource].
Published
Washington, D.C. : U.S. Atomic Energy Commission, 1966. Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy
The slow decay of naturally occurring radioactive elements in the earth's crust has ticked off the seconds with unalterable precision since the earth was born. Thus by measuring the amount of the elements' decay we can determine the age of the material of which they are a part. The first purpose of the work in this thesis was to seek additional criteria which may be applied to fossil marine mollusks as tests of closed system conditions. The second purpose was to apply these criteria to two series of well preserved fossil marine mollusks.