A new evaluation of the elastic thickness (Te) structure of the Indian Shield, derived from isotropic fan wavelet methodology, documents spatial variations of lithospheric deformation in different tectonic provinces correlated with episodic tectono-thermal events. The Te variations corroborated by shear velocity, crustal thickness, and seismogenic thickness reveal the heterogeneous rheology of the Indian lithosphere. The thinned, attenuated lithosphere beneath Peninsular India is considered to be the reason for its mechanically weak strength (<30 km), where a decoupled crust-mantle rheology under different surface/subsurface loading structures may explain the prominent low Te patterns. The arcuate Te structure of the Western Dharwar provinc...
Analysis of data from nine, temporary broadband seismic stations operated across West Bengal and Sik...
Due to the paucity of seismological data available in the public domain, the structure of the Indian...
The major scientific purpose of this work is to evaluate the geodynamic processes involved in the de...
A new evaluation of the elastic thickness (Te) structure of the Indian Shield, derived from isotropi...
The elastic thickness (Te) of continents is a matter of much debate. Recent studies have shown that ...
We use the Bouguer coherence (Morlet isostatic response function) technique to compute the spatial v...
The nature of crustal and lithospheric mantle evolution of the Archean shields as well as their subs...
AbstractThe nature of crustal and lithospheric mantle evolution of the Archean shields as well as th...
The Satpura Mountain Belt, or the Central Indian Tectonic Zone (CITZ), is a Paleoproterozoic mountai...
The chief elements in the structure of the earth's crust are shield and stable areas (platforms), se...
This paper is concerned with the implications of earthquake depth distributions in the Himalayan–Tib...
Analysis of several geophysical signatures yields a new model for the south Indian continental litho...
The flexural bulge in central India resulting from India’s collision with Tibet has a wavelength of ...
The flexural bulge in central India resulting from India's collision with Tibet has a wavelengt...
We present a high-resolution 3-D lithospheric model of the Indian plate region down to 300 km depth,...
Analysis of data from nine, temporary broadband seismic stations operated across West Bengal and Sik...
Due to the paucity of seismological data available in the public domain, the structure of the Indian...
The major scientific purpose of this work is to evaluate the geodynamic processes involved in the de...
A new evaluation of the elastic thickness (Te) structure of the Indian Shield, derived from isotropi...
The elastic thickness (Te) of continents is a matter of much debate. Recent studies have shown that ...
We use the Bouguer coherence (Morlet isostatic response function) technique to compute the spatial v...
The nature of crustal and lithospheric mantle evolution of the Archean shields as well as their subs...
AbstractThe nature of crustal and lithospheric mantle evolution of the Archean shields as well as th...
The Satpura Mountain Belt, or the Central Indian Tectonic Zone (CITZ), is a Paleoproterozoic mountai...
The chief elements in the structure of the earth's crust are shield and stable areas (platforms), se...
This paper is concerned with the implications of earthquake depth distributions in the Himalayan–Tib...
Analysis of several geophysical signatures yields a new model for the south Indian continental litho...
The flexural bulge in central India resulting from India’s collision with Tibet has a wavelength of ...
The flexural bulge in central India resulting from India's collision with Tibet has a wavelengt...
We present a high-resolution 3-D lithospheric model of the Indian plate region down to 300 km depth,...
Analysis of data from nine, temporary broadband seismic stations operated across West Bengal and Sik...
Due to the paucity of seismological data available in the public domain, the structure of the Indian...
The major scientific purpose of this work is to evaluate the geodynamic processes involved in the de...