000			02044cam a2200373 a 4500
003			EG-NbEJU
005			20240717094448.0
008			240717s1992 us a grb 001 0 eng d
010			_a2006018348
020			_a0931830567 (Series)
020			_a1560800585 (Volume)
035			_a(OCoLC)ocm69792173
035			_a(OCoLC)69792173
040			_aEG-NbEJU _cEG-NbEJU _dEG-NbEJU _beng
041			_aeng
050	0	0	_aQC809 _b.E15W48 1992
100	1		_aWhittall , Kenneth Patrick , _d1955-
245	1	0	_aInversion of Magnetotelluric data for a One-dimensional Conductivity / _cby : Kenneth P. Whittall and Douglas W. Oldenburg
260			_aOklahoma , United Stste of America : _bThe Society of Exploration Geophysics , _c1992
300			_av , 114 pages : _billustrations ; _c24 cm.
490	0		_aGeophysical monograph series ; _vno. 5
500			_aNumber 5 : Inversion of Magnetotelluric Data for a One-Dimensional Conductivity by : Kenneth P. Whittall and Douglas W. Oldenburg
504			_aIncludes bibliographical references and index
520			_aThe magnetotelluric (MT) method, pioneered by Tikhonov (1950) and Cagniard (1953), has been applied with varying degrees of success to yield information about the Earth's electrical conductivity, temperature regimes, and geologic structure. The strengths and weaknesses of the MT method are now generally appreciated and the majority of research over the past few years has concentrated on data processing, forward modeling and inversion. Historically, MT interpretation has used one-dimensional (1-D) forward modeling algorithms, 1-D inversions, and 2-D forward modeling
650		7	_aEarth Resistance _2LCSH _xMeasurement
650		7	_aInverse Problems (Different Equations) _2LCSH
650		7	_aContinuum mechanics _vTextbooks _2LCSH
700	1		_aOldenburg , Douglas W. , _d1946- _eco-author
700	1		_aFitterman , David V. , _eEditor of series
830		0	_aGeophysical monograph series ; _vno. 5
901			_asara sorur
902			_aENG_03_ (2358)
942			_2lcc _cBK
999			_c3941 _d3941