Abstract
THE Mountsorrel granodiorite1–3 is situated 7 miles north of Leicester. The intrusion is boss-like in form, about a mile in diameter, and is considered to be Caledonian as it has an isotopic age of 403 ± 18 m.y.4,5. The mineralization which occurred within the granodiorite after consolidation has been studied by many workers; the most recent is King6, who subdivided the mineralization into five stages, the first two being pneumatolytic and the others hydrothermal.
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 callSimilar Papers
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.
