Abstract
Stable isotopes in crystalline materials under certain conditions (e.g., at high pressures in interior of planets) can form ordered (in space) or correlated distributions. There are several experimental methods that can be upgraded for the search of the positional isotopic correlations (IC) and isotopic superlattices. Differences in the degree of IC in natural crystallites, if detected, could be interpreted as indicators of their formation history. Therefore, a search for IC could open a new application of isotopic geology complementary to the detection of variations of isotopic abundances in minerals, rocks and meteorites.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
