Moho depth across the Trans-European Suture Zone from P- and S-receiver functions

Moho depth variation in southern California from teleseismic receiver functions

The number of broa.dband three-component seismic stations in southern California. has more tb an tripled recently. In th is study we use the teleseismic receiver function technique to determine the crustal thicknesses and Vp / Vs ratios for th ese stations and map out t he lateral variation of Moho dept h under southern California. It is shown t hat a. receiver function can provide a very good ...

Moho depth variation in Taiwan from teleseismic receiver functions

moho depth and vp/vs variations in the kope dagh region from analysis of teleseismic receiver functions

in this study we use the p receiver function technique to determine the moho depth and vp/vs ratio for 8 short period stations of qochan and mashhad seismic networks and map the variations of moho depth under kope dagh region. it is shown that a receiver function can provide a relatively good point measurement of moho depth under a short period station. the crustal thickness estimated from the ...

moho depth and lithospheric thickness of the arabian and eurasian collision zone from potential field data

the targeted area of this research includes e anatoly, nw zagros, and caucasus. these structures are known as a complex and active area and in the early stage of continent-continent collision, which give us unique possibility to monitor such collision in real time. therefore, it is very important to study this active area to have a better knowledge about its tectonic behavior and lithospheric s...

Ten Kilometer Vertical Moho Offset and Shallow Velocity Contrast Along the Denali Fault Zone from Double-difference Tomography, Receiver Functions, and Fault Zone Head Waves