Tectonic setting of the northern terrane margin of the Eastern Ghats Mobile Belt: implication towards tectonics of juxtaposition between mobile belt and craton, and global correlation with Vestfold hills of Antarctica
Implementing Organization
Indian Institute of Technology (IIT)
Principal Investigator
Dr. Yengkhom Kesorjit singh
Indian Institute of Technology (IIT)
CO-Principal Investigator
Dr. syed Hilal Farooq
Indian Institute of Technology (IIT)
About
The Eastern Ghats Mobile Belt (EGMB) is surrounded by Archaean Cratons, including Dharwar Craton in the sW, Bastar Craton in the west, and NW and North Odisha-singhbhum Craton (NOsC) in the north. The contact between EGMB and these cratons is tectonic and marked by shear zones, such as the Terrane Boundry shear Zone (TBsZ). The NW margin is marked by the Lakhna thrust, associated with several nappes, and the NW front appears like a salient structure similar to the Phanerozoic thrust belt. The Paikamal lateral ramp continues eastward to join the Mahanadi shear zone of the EGMB. The northern margin of the EGMB with the North Odisha singbhum Craton is marked by a set of strike-slip shear zones, possibly joining with the sukinda thrust. This study aims to study the kinematic and strain pattern of Barakot, sukinda, Riyamal, and Kerajang shear zones between Kamakhyanagar to Jaraka, which will shed light on the tectonics of juxtaposition Archaean and Proterozoic terranes in the eastern part of the Indian shield. The study will also identify multiple phases of nepheline syenite intrusion, geochemical analysis, and the formation and sedimentation of basins in the Mahanadi area.
Source
Source
science and Engineering Research Board (sERB), DsT
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