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 ...

This study aimed to investigate construct validity and factor structure of the Persian Occupational Self-Assessment (OSA; Baron, Kielhofner, Iyenger, Goldhammer, & Wolenski, 2003 ) based on the model of human occupation (MOHO). Three hundred and thirty-six (179 male and 157 female) Iranian junior high students were measured using the OSA. The data were analyzed using a Confirmatory Factor Analy...

Since its discovery in 1909, the Moho was routinely studied by seismological methods. However, from 1950s, a possible alternative introduced gravimetric inversion. Thanks to satellite gravity missions launched beginning of 21st century, global inversion became feasible, e.g., leading computation GEMMA model 2012. This computed inverting GOCE second radial derivatives anomalous potential Wiener ...

We develop an algorithm for a Moho depth recovery from gravity and gradiometry data apply this method to estimate the beneath Tibetan Plateau. The basic idea of is describe mathematically undulations in terms condensation layer with respect mean depth, instead applying more commonly used isostatic compensation schemes. Expressions that functionally relate field quantities (Moho) are derived spe...

Abstract In this study, we present a new Moho depth model in Fennoscandia and its surroundings. The is tailored from data sets of XGM2019e gravitationl field, Earth2014 topography seismic crustal CRUST1.0 using the Vening Meinesz-Moritz based on isostatic theory to resolution 1° × 1°. To that end, refined Bouguer gravity disturbance determined by reducing observed field for effect topography, d...

We develop the theoretical foundations, numerical algorithms and computer programs to retrieve the 3D geometry of a density interface from gridded gravity data. The solution depends on constraining assumptions on permissible density values. An integral equation is solved by a new method of local corrections to find the density interface. The method is efficient and does not require trial-and-er...