Abstract
ABSTRACT Laminations are described from a sequence of marine shales in the Yorkshire Coal Measures. Variations in the thickness of the laminae through the sequence have been noted and also the changes in composition between the light and dark laminae. Based on the observed changes it has been deduced that the laminae are valves, and confirmation of this has been sought through a comparison with the varves in modern marine sediments.
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.
