Granitic Pegmatites, August 2012, Vol. 8, No. 4
June 28, 2024
Kaolin, June 2014, Vol. 10, No. 3
June 28, 2024
One Hundred Years Of Isotope Geochronology, February 2013, Vol. 9, No. 1
$20.00
In 1913, Frederick Soddy’s research on the fundamentals of radioactivity led to the discovery of “isotopes.” That same year, Arthur Holmes published his now famous booklet The Age of the Earth.
One Hundred Years Of Isotope Geochronology
February 2013, Vol. 9, No. 1
In 1913, Frederick Soddy’s research on the fundamentals of radioactivity led to the discovery of “isotopes.” That same year, Arthur Holmes published his now famous booklet The Age of the Earth. Combined, these two landmark events established the field of science we know as “isotope geochronology.” Today, isotope geochronology underpins much of our knowledge of the absolute age of minerals and rocks, and the records they contain. This field is constantly evolving, reflecting and responding to scientific drivers that require more highly resolved timescales, the microscopic analysis of smaller zoned minerals, or the generation of robust data sets in novel materials. This series of articles provides perspectives on the state of the art in the field of radioisotope dating—from the challenges of dating the Solar System’s oldest materials to resolving the record of Quaternary climate change, and the four and a half billion years in between.
Why You’ll Love Elements Magazine:
- Expert Contributors: Articles written by renowned researchers in the field of geoscience.
- Engaging Content: Join a community of readers who are passionate about Elements.
- Exceptional Quality: Each issue is printed on high-quality paper with stunning visuals and detailed illustrations that bring complex scientific concepts to life.
Order your copy of the February 2013 issue of Elements magazine today and learn about one hundred years of isotope geochronology.
Related products
-
Fluids in Planetary Systems, January 2005, Vol. 1, No. 1
$20.00Water and other geofluids play an important role in the geochemical and rheological evolution of the Earth and other bodies in the solar system. These fluids are responsible for the formation of hydrothermal mineral deposits, affect eruption behavior in volcanic systems and the geophysical properties of the mantle, and significantly affect the way in which rocks deform and fracture.
-
Frontiers In Textural And Microgeochemical Analysis, August 2007, Vol. 3, No. 4
$20.00Recent advances have been made in high-resolution in situ methods to image mineral growth patterns, analyse compositional and isotopic zonation, and improve our ability to visualize, study, and model rock textures in three dimensions. These advances provide a significant step forward in the understanding of how rocks form and the history they can tell us.
-
Arsenic, April 2006, Vol. 2, No. 2
$20.00Arsenic is an element known throughout history as a classic poison. Currently, very small but highly significant concentrations of this element in drinking water supplies are causing massive health problems to many millions of people in some of the world’s poorest nations, and more localised sources related to mining and processing are also a concern.
