Abstract
The Loon Lake batholith, which is supposed to be part of larger granitic masses underlying the Canadian Shield, was found to be a small, funnel-shaped intrusion. Its structure and shape is in complete accordance with the structure of the surrounding sediments and metamorphics.
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.
