We present a new crustal thickness map of the Chinese mainland and adjacent areas based
on a compilation of previously published data. More than 1900 estimates of crustal thickness …

This review presents an account of the variations in crustal and upper mantle structure
beneath the Indian subcontinent and its environs, with emphasis on passive seismic results …

We have used Bouguer gravity anomaly and topography data to determine the equivalent
elastic thickness of the lithosphere, Te in the region of the India–Eurasia collisional system …

Receiver functions are a powerful tool to isolate and interpret receiver-side structure effects
in teleseismic seismic records. They are easily constructed by deconvolving one component …

The S wave velocity structure of the crust and uppermost mantle of the Indian shield has
been investigated by jointly inverting P wave receiver functions and Rayleigh wave group …

The lithospheric structure of the Indian plate has been investigated using converted wave
techniques (P and S receiver functions) and a novel stacking analysis technique (without …

Peninsular India is traversed by several major Paleoproterozoic rift basins, among which the
Kaladgi rift basin is a prominent one. Here, we present results from Magnetotelluric (MT) …

The disintegration of the Columbia supercontinent during the late Paleoproterozoic
generated major rift basins in the constituent continental fragments. The Kaladgi basin …

The detection of a seismic boundary, the “Moho”, between the outermost shell of the Earth,
the Earth's crust, and the Earth's mantle by A. Mohorovičić was the consequence of …

Peninsular India is a cratonic region with asymmetric relief manifest by eastward tilting from
the 1.5 km high Western Ghats escarpment toward the floodplains of eastward‐draining …