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| 003 | MX-MdCICY | ||
| 005 | 20250625160150.0 | ||
| 040 | _cCICY | ||
| 090 | _aB-16393 | ||
| 245 | 1 | 0 | _aRapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method |
| 490 | 0 | _vGeophysical Prospecting, 44(1), p.131-152, 1996 | |
| 520 | 3 | _aA fast inversion technique for the interpretation of data from resistivity tomography surveys has been developed for operation on a microcomputer. This technique is based on the smoothness-constrained least-squares method and it produces a two-dimensional subsurface model from the apparent resistivity pseudosection. In the first iteration, a homogeneous earth model is used as the starting model for which the apparent resistivity partial derivative values can be calculated analytically. For subsequent iterations, a quasi-Newton method is used to estimate the partial derivatives which reduces the computer time and memory space required by about eight and twelve times, respectively, compared to the conventional least-squares method. Tests with a variety of computer models and data from field surveys show that this technique is insensitive to random noise and converges rapidly. This technique takes about one minute to invert a single data set on an 80486DX microcomputer. | |
| 650 | 1 | 4 | _aCOMPUTER SIMULATION |
| 650 | 1 | 4 | _aELECTRIC CONDUCTIVITY OF SOLIDS |
| 650 | 1 | 4 | _aINVERSE KINEMATICS |
| 650 | 1 | 4 | _aITERATIVE METHODS |
| 650 | 1 | 4 | _aLEAST SQUARES APPROXIMATIONS |
| 650 | 1 | 4 | _aMATHEMATICAL MODELS |
| 650 | 1 | 4 | _aMICROCOMPUTERS |
| 650 | 1 | 4 | _aPARTIAL DIFFERENTIAL EQUATIONS |
| 650 | 1 | 4 | _aRESPONSE TIME (COMPUTER SYSTEMS) |
| 650 | 1 | 4 | _aSPURIOUS SIGNAL NOISE |
| 650 | 1 | 4 | _aSURFACE PROPERTIES |
| 700 | 1 | 2 | _aLoke, M.H. |
| 700 | 1 | 2 | _aBarker, R.D. |
| 856 | 4 | 0 |
_uhttps://drive.google.com/file/d/1Kq5OWDoLK0l9DNCrnl0Gq3jR5hTKtL4w/view?usp=drivesdk _zPara ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx |
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