Abstract
A method for determination of the relative geological age of subaqueous Quaternary deposits is proposed. It is based on the evaluation of the ratio of fluorescence intensity at 450 nm to the optical density of muriatic solution extracted out of a carbonaceous fossil shell.
Sign-in/Register to access full text options 
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 callMore From: Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine
Disclaimer: 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.
