radiogenic's Usage Examples:

A radiogenic nuclide is a nuclide that is produced by a process of radioactive decay.

variations arising from mass-dependent isotope fractionation, whereas radiogenic isotope geochemistry is concerned with the products of natural radioactivity.

on the radioactive decay of a long-lived samarium isotope (147Sm) to a radiogenic neodymium isotope (143Nd).

40Ar* refers to the radiogenic 40Ar, i.

terawatts (TW) and comes from two main sources in roughly equal amounts: the radiogenic heat produced by the radioactive decay of isotopes in the mantle and crust.

dated by measurement of the concentration of potassium and the amount of radiogenic 40Ar that has accumulated.

Theoretically, such stable isotopes could include the radiogenic daughter products of radioactive decay, used in radiometric dating.

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

isotope as a daughter of natural radioactive isotopes (as in the case of radiogenic isotopes of lead).

to a “radiogenic” daughter isotope.

Changes in the parent/daughter ratio by, for example, mantle melting, results in changes in the radiogenic isotopic.

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.

Lead-204 is entirely a primordial nuclide and is not a radiogenic nuclide.

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

On the other hand, radiogenic isotope analysis involves measuring the abundances of decay-products of.

third, after 232Th and 238U, as the source of radiogenic heat.

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

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

The stable argon isotope 40Ar is actually more common as a radiogenic nuclide.

deposits will contain no lead, meaning that any lead found in the mineral is radiogenic.

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

Together these decay chains account for more than 99% of the present-day radiogenic heat generated inside the Earth.

53Cr is the radiogenic decay product of 53Mn.