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Petrography and tectonic provenance of the tertiary rocks of changki valley, mokokchung district, nagaland, northeast India

Author: 
Ralimongla and Pandey, N.
Subject Area: 
Social Sciences and Humanities
Abstract: 

The Tertiary rocks of Changki Valley constitute a part of belt of Schuppen - a most prominent morphotectonic unit of Naga Hills stretching along the western margin of Nagaland State. The Barail Group (Tikak Parbat Formation), Changki Formation and Tipam Group (Tipam Sandstone Formation) have been studied for their petrographic features and tectonic provenance. Based on the study, it may be inferred that the Tertiary sediments under question are mostly lithic in nature and received their detritus from a recycled orogen , especially the collision orogen provenances. The coal bearing Tikak Parbat Formation appears to have derived its detritus from the newly risen NHO to the east as well as the newly uplifted Himalaya and Trans – Himalayas to the north. The Changki Formation calls for a foreland uplift province besides recycled orogen whereas a collision orogen provenance together with uplifted igneous & metamorphic terrenes adjacent to the crustal suture may be assigned to the Tipam Sandstone Formation.

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