Abstract
The Old Red Sandstone lavas of the Eastern Sidlaws are described. Olivine-basalts predominate. There are also a number of two-pyroxene basalts of which two have been chemically analysed. Comparisons are made with other Old Red Sandstone lavas in adjacent areas. It is seen that the lava suite of the whole Sidlaw range is predominantly basic in character.
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 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.
