Most of the convergence in the Lesser Himalaya of Garhwal and Kumaon is being accommodated just south of the Main Central Thrust fault trace, indicating high strain accumulation in this region which is also consistent with the high seismic activity in this region. In addition, for the first time an arc-normal extension of ?6 mm/year has also been observed in the Tethyan Himalaya of Kumaon.
Contemporary deformation in the Kashmir–Himachal, Garhwal and Kumaon Himalaya: significant insights from 1995–2008 GPS time series. Springer Berlin Heidelberg, 2014 с. 539 - 557,.
Contemporary deformation in the Kashmir–Himachal, Garhwal and Kumaon Himalaya: significant insights from 1995–2008 GPS time series. Springer Berlin Heidelberg, 2014 с. 539 - 557,.
(2014) Contemporary deformation in the Kashmir–Himachal, Garhwal and Kumaon Himalaya: significant insights from 1995–2008 GPS time series, Springer Berlin Heidelberg с. 539 - 557,.
(2014). Contemporary deformation in the Kashmir–Himachal, Garhwal and Kumaon Himalaya: significant insights from 1995–2008 GPS time series. Springer Berlin Heidelberg, с. 539 - 557.
Contemporary deformation in the Kashmir–Himachal, Garhwal and Kumaon Himalaya: significant insights from 1995–2008 GPS time series. Springer Berlin Heidelberg; 2014. p. с. 539 - 557.
