Abstract
An effective method for identifying tectonic-magmatic causes of metamorphism is the reconstruction and analysis of P – T – t paths, which can be used to develop a tectonic model of rock evolution with time. Diagnostic P-T-t paths characteristic of rocks formed in zones of active tectogenesis – under collision, extension and in shear zones of the earth’s crust – have been established. This report discusses some of the ambiguous interpretations of P-T-t paths in areas with simultaneous manifestation of different metamorphic processes.
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: Proceedings of the Karelian Research Centre of the Russian Academy of Sciences
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.
