Noun
(geology, geochemistry) A line on a chart linking rock of the same age (as determined from isotope ratios).
(mathematics, dynamical systems) A collection of points (such as a manifold), each point representing a set of initial conditions for a given dynamical system, such that every set results in the same long-term behaviour of the system.
Source: en.wiktionary.orgPlotting an isochron is used to solve the age equation graphically and calculate the age of the sample and the original composition. Source: Internet
The age is calculated from the slope of the isochron (line) and the original composition from the intercept of the isochron with the y-axis. Source: Internet
The iodine-xenon chronometer citation is an isochron technique. Source: Internet