The history of Earth in the Solar System has been unraveled
using natural radioactivity. The sources of this radioactivity are
the original creation of the elements and the subsequent
bombardment of objects, including Earth, in the Solar System by
cosmic rays. Both radioactive and radiogenic nuclides are harnessed
to arrive at ages of various events and processes on Earth.
This collection of chapters from the Treatise on Geochemistry
displays the range of radioactive geochronometric studies that have
been addressed by researchers in various fields of Earth science.
These range from the age of Earth and the Solar System to the
dating of the history of Earth that assists us in defining the
major events in Earth history. In addition, the use of radioactive
geochronometry in describing rates of Earth surface processes,
including the climate history recorded in ocean sediments and the
patterns of circulation of the fluid Earth, has extended the range
of utility of radioactive isotopes as chronometric and tracer
tools.
Comprehensive, interdisciplinary and authoritative content selected
by leading subject expertsRobust illustrations, figures and
tablesAffordably priced sampling ofcontent from the full "Treatise
on Geochemistry""
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