radiogenic's Usage Examples:

signature (also isotopic fingerprint) is a ratio of non-radiogenic "stable isotopes", stable radiogenic isotopes, or unstable radioactive isotopes of particular.

isotope (147Sm) to a radiogenic neodymium isotope (143Nd).

Of naturally occurring radioisotopes, the most stable is radiogenic 210Bi with a half-life of 5.

Stable isotope tracers involve only non-radiogenic isotopes and usually.

Therefore, given sufficient time for significant production (ingrowth) of radiogenic 87Sr, measured 87Sr/86Sr values will be different in the.

An isotopic signature (also isotopic fingerprint) is a ratio of non-radiogenic "stable isotopes", stable radiogenic isotopes, or unstable radioactive.

source of the rock or rocks contained unknown amounts of both radiogenic and non-radiogenic isotopes of the daughter element, along with some amount of.

subdivided into two categories: stable isotope tracers and radiogenic isotope tracers.

all radiogenic nuclide daughters of uranium decay and are found in uranium ores.

The core also likely contains radiogenic sources, although how much is uncertain.

53Cr is the radiogenic decay product of 53Mn.

The radiogenic daughter, 87Sr, is produced in this decay process and was produced in.

to a “radiogenic” daughter isotope.