A method of seismic traveltime inversion for simultaneous determination of 2-D velocity and
interface structure is presented that is applicable to any type of body-wave seismic data. The …

Strategies for modelling seismic refraction/wide-angle reflection traveltimes to obtain 2-D
velocity and interface structure are presented along with methods for assessing the reliability …

Seismic data represent one of the most valuable resources for investigating the internal
structure and composition of the earth. One of the first people to deduce earth structure from …

In the summer of 1998, project INDEPTH recorded a 400 km long NNW–SSE wide-angle
seismic profile in central Tibet, from the Lhasa terrane across the Banggong-Nujiang suture …

The International Deep Profiling of Tibet and the Himalaya Phase IV (INDEPTH IV) active
source seismic profile in northeast Tibet extends 270 km roughly north‐south across the …

Utilizing seismic refraction/wide-angle reflection data from 11 approximately in-line
earthquakes, 2-D P-and S-velocity models and a Poisson′ s ratio model of the crust and …

A tomographic inversion method is presented for the determination of 3-D velocity and
interface structure from a wide range of body-wave seismic traveltime data types. It is …

366 366 368 369 370 372 372 372 373 373 373 374 375 375 376 379 379 380 380 380
381 384 384 387 388 389 389 389 394 394 395 395 397 398 11.1 challenges in the form of …

We herein present a new seismic refraction/wide-angle reflection profile that crosses the
Songpan–Ganzi terrane, the Animaqing suture zone and the eastern Kunlun mountains …

An interface inversion has been tested and applied to wide‐angle reflection data from the
1986 PASSCAL Ouachita experiment. An interface corrugation with a relief of 10 km and a …