<p>Plate tectonic history of northeast Indian subcontinent can be viewed as a window to the<br>evolution of Southeast Asia. One such important tectonic feature is the northern most part of<br>Indo-Burmese Ranges where this research work has been carried out. Here we propose an<br>evolutionary model that shows northward moving &#8216;horse-tail&#8217; feature of the Hukawng Block<br>from the Burma basin, pushed this region towards the rigid Mishmi Block and Upper Assam<br>shelf, that caused the hyperoblique pattern of the ranges. It is the juxtaposition of the three<br>continental blocks: India-Asia-Burma, where there are tectonic and geomorphic influences in<br>the Block from both the Himalayan and Indo-Burmese orogeny. Stress distribution among<br>north-easterly moving Indian plate and comparatively stiff Eurasian and Burma plates, within<br>the India specific reference frame, is resulting in further changes. The study area mainly falls<br>under Changlang district of Arunachal Pradesh, India; and the regional study has been done in<br>the quadrangle from 26&#176; to 28&#176;N in latitudes and 95&#176; to 97&#176;E in longitudes. Morphotectonic<br>study, lineament analysis, fault system characterisation, focal plane mechanism along with<br>dynamic topography, seismic tomography and gravity anomaly have been incorporated in the<br>field evidences. Morphotectonic study for Noa-Dihing River basin has resulted in a value of<br>56.59 for Asymmetric Factor, which shows similar asymmetry result like in the Chi (&#967;)<br>analysis. This SW-ward tilted basin is moderately asymmetrical with Transverse Topographic<br>Symmetric Factor value of 0.42. This indicates that the major river basin along with other subbasins<br>are under the influence of active oblique rotational component. The regional lineaments<br>are showing mean orientations of N11&#176;E-S11&#176;W, N70&#176;W-S70&#176;E and EW whereas some local<br>trends of minor lineaments, in some places have mean orientations of N40&#176;W-S40&#176;E, N82&#176;WS82&#176;<br>E and N42&#176;E-S42&#176;W. In Mishmi block the major regional trends are N35&#176;W-S35&#176;E and<br>N40&#176;E-S40&#176;W comprising of probable cross-faults. In Hukawng Block, the lineament<br>orientation changes from N50&#176;W-S50&#176;E in the west to N30&#176;W-S30&#176;E, N-S and N15&#176;E-S15&#176;W<br>in the central valley region (north of Jade mines) and then to N50&#176;E-S50&#176;W in the eastern side.<br>Major fault systems are mostly thrust, with some showing very low angle slip component,<br>along with some oblique slip faults (e.g. Noa-Dihing River). The dynamic topography and<br>seismic tomographic studies indicate presence of a high seismic velocity zone beneath Mishmi<br>block indicating the crystalline rock materials. The block is still actively exhuming. Moreover,<br>Changlang and Hukawng blocks have undergone uplift and then phases of subsidence during<br>the last 20Ma. This indicates that the Low Velocity materials that are present underneath were<br>subjected to some crustal deformations. This tectonic process has also resulted in gravity<br>anomalies. The role of massive and rigid Mishmi block, comprising older crystalline rocks and,<br>later forming Burma basins formed the oblique rotation of the Changlang block which is<br>observed from all stated methods. Hukawng Block, which is controlled by the motion of<br>Sagaing Fault, have influenced the Changlang Block by its varied strike-slip stress components.<br>Moreover, Indo-Burmese Ranges also has an influence on this block and vice-versa.</p>