Abstract
Jonk river conglomerate occurs along the river Jonk of the late Archean-Paleoproterozoic Sonakhan greenstone belt in the northern-eastern part of the central India craton (CIC)/Bastar block of Central India. To quantify finite strain, the Rf/f and Fry techniques were used. For the 3D strain analysis, conventional Flinn diagram was computed, on which variation of finite strain as computed from harmonic mean for the different localities, that most of the pebble shapes designates at the oblate field and have nearly plain strain ellipsoid.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
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.