[et_pb_section bb_built=”1″ admin_label=”section” _builder_version=”3.0.47″ custom_padding=”19px|0px|0px|0px”][et_pb_row admin_label=”row” _builder_version=”3.0.47″ background_size=”initial” background_position=”top_left” background_repeat=”repeat” custom_padding=”0px|0px|28.95px|0px”][et_pb_column type=”4_4″][et_pb_text _builder_version=”3.0.102″ background_size=”initial” background_position=”top_left” background_repeat=”repeat” background_layout=”light”]<\/p>\n
Software<\/strong><\/em><\/span><\/td>\n| Author<\/strong><\/em><\/span><\/td>\n | Platform<\/strong><\/em><\/span><\/td>\n | Short description<\/strong><\/em><\/span><\/td>\n<\/tr>\n | ANRAY<\/a><\/td>\n | Ivan P\u0161en\u010d\u00edk<\/td>\n | \u00a0fortran<\/td>\n | Computation of rays, travel times, ray amplitudes and ray synthetic seismograms in 3-D laterally varying structures with isotropic and\/or generally anisotropic layers.<\/td>\n<\/tr>\n | SEIS88<\/a><\/td>\n | Ivan P\u0161en\u010d\u00edk<\/td>\n | \u00a0fortran<\/td>\n | Computation of rays, travel times, ray amplitudes and ray synthetic seismograms in 2-D laterally varying layered isotropic structures.<\/td>\n<\/tr>\n | ANNI<\/a> (Matlab) | \nANNI (Scilab)<\/td>\n Bohuslav R\u016f\u017eek<\/td>\n | Matlab, Scilab<\/td>\n | Artifitial Neural Network Inversion Tool for Matlab and Scilab.<\/td>\n<\/tr>\n | rmseed<\/a><\/td>\n | Bohuslav R\u016f\u017eek<\/td>\n | Matlab, Scilab<\/td>\n | Program for reading binary seismic data written in MiniSEED format for Matlab and Scilab<\/td>\n<\/tr>\n | SPLITshear<\/a><\/td>\n | Lud\u011bk Vecsey<\/td>\n | Matlab, fortran<\/td>\n | Splitting evaluation program. Graphical interface enables proper setting of a window of analyzed signal. Three methods are available for splitting parameters evaluation: cross-correlation, eigenvalue and transverse minimization. Error estimation is implemented by the bootstrap method.<\/td>\n<\/tr>\n | MT_DECOMPOSITION<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/td>\n | \u00a0Matlab<\/td>\n | Matlab script on\u00a0 decomposition of seismic moment tensors (authentification required)<\/td>\n<\/tr>\n | PCA-DECOMPOSITION<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/td>\n | \u00a0Matlab<\/td>\n | Matlab script on calculating common wavelet from seismic traces based on the Principal Component Analysis<\/td>\n<\/tr>\n | Plot_mechanism<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/td>\n | \u00a0Matlab<\/td>\n | Matlab script on plotting non-double-couple mechanisms from full seismic moment tensors.<\/td>\n<\/tr>\n | Thompsen_par<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/td>\n | \u00a0Matlab<\/td>\n | Matlab script on calculating elastic parameters describing a weakly transversely isotropic medium from Thomsen’s parameters and vice versa.<\/td>\n<\/tr>\n | STRESSINVERSE<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/td>\n | Matlab, Python<\/td>\n | Software for the stress inversion (authentification required)<\/td>\n<\/tr>\n | SYMMETRY<\/a><\/td>\n | V\u00e1clav Vavry\u010duk<\/p>\n | Ali Aminzadeh<\/td>\n Matlab<\/td>\n | Software for identification of anisotropic symmetry (authentification required)<\/td>\n<\/tr>\n | amp_rat_inv<\/td>\n | Zuzana Jechumt\u00e1lov\u00e1<\/td>\n | <\/td>\n | The Fortran computer program performs inversion of amplitude ratios of\u00a0 SH and SV seismic waves together with polarities of P waves into the mechanism of the seismic source in the description of unconstrained moment tensor (MT). As such, it allows describe general dipole sources including isotropic components: e.g., it is suitable to retrieve the parameters of both a shear dislocation common at foci of tectonic earthquakes (described as a double-couple, DC) and volumetric sources as tensile cracks or cavity implosions.<\/td>\n<\/tr>\n | amp_inv_rot<\/td>\n | Zuzana Jechumt\u00e1lov\u00e1<\/td>\n | <\/td>\n | The Fortran computer program retrieves source mechanisms of seismic events observed from a single (vertical or near vertical) array of receivers. This single-azimuth dataset cannot resolve the dipole perpendicular to the plane of stations and the hypocenter. Because of this program inverts only for the moment tensor components that are constrained by the observed data and gives a set of source mechanisms fitting the data.<\/td>\n<\/tr>\n | Demo Area Move<\/a><\/td>\n | Petr Kol\u00e1\u0159<\/td>\n | Matlab<\/td>\n | Demo MATLAB code to interactively move\/resize selected area in a figure.<\/td>\n<\/tr>\n | Demo Repeat Button<\/a><\/td>\n | Petr Kol\u00e1\u0159<\/td>\n | Matlab<\/td>\n | Repeated a callback function of a button (`togglebutton\u00b4) while the button is pressed.<\/td>\n<\/tr>\n | Demo Slider<\/a><\/td>\n | Petr Kol\u00e1\u0159<\/td>\n | Matlab<\/td>\n | Demo MATLAB code for better control of a zoomed figure.<\/td>\n<\/tr>\n | TELINV2012<\/td>\n | J.Taylor, E.Kissling, U.Achauer, C.M.Weiland, L.Steck, H.Shomali and others<\/p>\n | Revidov\u00e1no Hanou Karousovou a Helenou Munzarovou<\/td>\n fortran, Matlab<\/td>\n | TELINV2012 is a code for calculation of velocity perturbations relative to 1D Earth velocity model from relative travel-time residuals. The code enables 1D or3D ray tracing. The latter one is implemented according to the Simplex ray-tracing technique. The velocity perturbations are searched at nodes among which velocities are linearly interpolated. The velocity perturbations are calculated in subsequent iteration steps, in which the ray paths and travel-time residuals are updated. A part of the TELINV2012 package is a manual and auxiliary GMT, Matlab and Fortran scripts for simple visualization of input data and model parameters and for preparation of input \u001cfiles.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n | [\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":" Software Author Platform Short description ANRAY Ivan P\u0161en\u010d\u00edk \u00a0fortran Computation of rays, travel times, ray amplitudes and ray synthetic seismograms in 3-D laterally varying structures with isotropic and\/or generally anisotropic layers. SEIS88 Ivan P\u0161en\u010d\u00edk \u00a0fortran Computation of rays, travel times, ray amplitudes and ray synthetic seismograms in 2-D laterally varying layered isotropic structures. ANNI (Matlab) […]<\/p>\n","protected":false},"author":4,"featured_media":3827,"parent":404,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-7916","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"\n |