# Pure and Applied Geophysics

Pure and Applied Geophysics > 2005 > 162 > 1 > 21-36

*(γ*

_{ R }) predicted by previously determined frequency-independent models of shear-wave Q (

*Q*

_{ μ }), we have obtained frequency-dependent

*Q*

_{ μ }models that explain measured values of γ

_{ R }as well as of Lg coda

*Q*and its frequency dependence at 1 Hz (

*Q*

_{ o }and

*η*, respectively) for China and some adjacent regions. The process...

Pure and Applied Geophysics > 2005 > 162 > 1 > 91-107

*M*< 3.0), through moderate (

*M*<

*M*

_{ c }, where...

Pure and Applied Geophysics > 2005 > 162 > 1 > 145-164

Pure and Applied Geophysics > 2005 > 162 > 1 > 129-144

*P*

_{ n }velocity and Curie point depth, which are temperature dependent.

*P*

_{ n }velocity has been determined by reanalyzing deep seismic sounding (DSS) records obtained for this region. Surface heat flow has been computed using the

*P*

_{ n }velocity data from...

Pure and Applied Geophysics > 2005 > 162 > 1 > 109-128

^{th}century and lasting until...

Pure and Applied Geophysics > 2005 > 162 > 1 > 1-20

*M*7.3 Chi-Chi earthquake sequence including the main shock and some aftershocks. The four-level array (0 m, 50 m, 100 m and 200 m) is located to the north of Hualien City in eastern Taiwan. Polarization analysis is used to check the orientation errors of the seismometers at different...

Pure and Applied Geophysics > 2005 > 162 > 1 > 165-179

Pure and Applied Geophysics > 2005 > 162 > 1 > 73-90

*b*value (decrease) and fractal dimensions (decrease in both

*D*

_{2}

^{s}and D

_{2}

^{t}) of earthquake epicenters 0.5 and 2.5 years prior to 1973 (

*M*5.2) and 1980 (

*M*5.5) events, respectively, except a negative correlation for about five years (1988–1993) prior to the 1993/1994 sequence...

Pure and Applied Geophysics > 2005 > 162 > 1 > 181-200

Pure and Applied Geophysics > 2005 > 162 > 1 > 53-72

*M*

_{ w }7.7 of 26 January, 2001 took place along the south-dipping reverse fault in the lower crust (∼ 23 km) of Kutch, Gujarat, India, obliterating some 14,000 people. The aftershock activity has ensued for three years. We analyzed 997 aftershocks of

*M*≥ 3.0 to study the

*b*value and fractal correlation dimensions in time and space. The ‘

*b*’ value is found to...

Pure and Applied Geophysics > 2005 > 162 > 1 > 37-51

*P*-wave travel time inversion, applying a two-step tomography procedure. The data set consists of the travel-time residuals of 584 well located earthquakes. In order to improve the initial (reference) velocity model, before the inversion of travel times, the “minimum 1-D” model was determined...

Pure and Applied Geophysics > 2005 > 162 > 2 > 221-248

^{3}of brine...

Pure and Applied Geophysics > 2005 > 162 > 2 > 409-431

Pure and Applied Geophysics > 2005 > 162 > 2 > 249-271

Pure and Applied Geophysics > 2005 > 162 > 2 > 291-310

*M*

_{ w }> 7.1 earthquakes along high-angle reverse faults. We have modeled induced changes in Coulomb failure stress (ΔCFS) to determine whether stress triggering could have occurred during the 1929 and 1968 sequences and to determine how these earthquakes have affected stress along the Alpine...

Pure and Applied Geophysics > 2005 > 162 > 2 > 273-289

Pure and Applied Geophysics > 2005 > 162 > 2 > 373-407

Pure and Applied Geophysics > 2005 > 162 > 2 > 357-371

*et al.*(1985). The Curie point depth of central Anatolia varies from 7.9 km and 22.6 km. The shallowest...