Tertiary rocks of Changkikong Range constitutes a part of belt of Schuppen- a most prominent morphotectonic unit of Naga Hills. The palaeocurrent patterns for the Barail Group (Tikak Parbat Formation) , Changki Formation and Tipam Group (Tipam Sandstone Formation) have been studied . Interpretation reveals polymodal, bimodal , bimodal-pipolar palaeocurrent patterns in the study area.
Dr. Ralimongla (2018); Palaeocurrent Analysis of the Tertiary Rocks of Changkikong Range, Mokokchung District, Nagaland, Northeast India; International Journal of Scientific and Research Publications (IJSRP)
8(8) (ISSN: 2250-3153), DOI: http://dx.doi.org/10.29322/IJSRP.8.8.2018.p8046