©Sandmeier Scientific Software 2012
the complete 2D processing and
software with modular arrangement for
With more than 1000 licences Reflexw is one of the world's most popular geophysical near surface processing and interpretation packages.
Reflexw has a modular character. Therefore you may assemble your own modular arrangement regarding your personal needs.
This crosstable gives you a summary of the useful combinations of the available module and the individual applications.
Short overview of the different Reflexw modules
easy generation of a 3D-dataset from individual 2D-lines which may be parallel, crossing or randomly spaced wihtin the xy-plane
x-,y- or z-slices
. The slices are either displayed in manually scalable windows or by moving through the 3D-dataset using a track bar
of the individual slices or of the full 3D-data using shading algorithms
refraction traveltime analysis
for refraction seismics
Interpretation of refraction seismic
. The module includes various
sorting and combining possibilities for
the picked traveltimes.
These combined traveltimes are the bases
for a FD based
interactive 1D-velocity analysis
allows the adaptation of the complete
traveltime branch including diving waves.
methods are available
for the evaluation of synthetic traveltimes.
based on SIRT
is incorporated for the inversion of the
for simulating the electromagnetic and seismic wave propagation in a 2-dimensional medium using a
Finite Difference scheme
approach based on
is incorporated for the inversion of the picked traveltimes (refraction and transmission). Straight and curved rays are supported.
of data of many different formats (e.g. SEGY, SEG2, most of the GPR- and seismic systems (GSSI, RAMAC, PULSE-EKKO, ABEM, OYO, Summit, IDS, UTSI and so on)), integration of other non-standard formats.
possibilities - interactive processing of single files or by generating a batch-file, one- and multi-channel filters, editing, static correction, deconvolution, migration and much more. All processing steps are documented.
of diffractions or first arrivals giving an estimate of the average velocities
of arrivals - manual, automatic or semi-automatic, ASCII-conversion of the picks
(sorting, display, processing, NMO-analysis, stacking)
of CMP- or shot-data using a semblance analysis or an interactive adaptation method calculating either the reflection hyperbolas (reflection seismics) or the complete traveltime branch including diving waves (refraction seismics).
Dr. Karl-Josef Sandmeier, Zipser Strasse 1, 76227 Karlsruhe, Germany
Tel. ++49-721-491206, Fax ++49-721-4067994, e-mail: firstname.lastname@example.org