000			03134nam a22005295i 4500
001			978-3-540-77814-1
003			DE-He213
005			20161121230921.0
007			cr nn 008mamaa
008			100715s2008 gw | s |||| 0|eng d
020			_a9783540778141 _9978-3-540-77814-1
024	7		_a10.1007/978-3-540-77814-1 _2doi
050		4	_aQC801-809
072		7	_aPHVG _2bicssc
072		7	_aSCI032000 _2bisacsh
082	0	4	_a550 _223
082	0	4	_a526.1 _223
100	1		_aBerdichevsky, Mark N. _eauthor.
245	1	0	_aModels and Methods of Magnetotellurics _h[electronic resource] / _cby Mark N. Berdichevsky, Vladimir I. Dmitriev.
264		1	_aBerlin, Heidelberg : _bSpringer Berlin Heidelberg, _c2008.
300			_aX, 564 p. 551 illus. _bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_aonline resource _bcr _2rdacarrier
347			_atext file _bPDF _2rda
505	0		_aMagnetotelluric and Magnetovariational Response Functions -- The Magnetotelluric Response Functions -- The Impedance Eigenstate Problem -- Separation of the Local and Regional Magnetotelluric Effects -- The Magnetovariational Response Functions -- The Recent Developments -- Basic Models of the Distortion Theory -- Two Classic Models of the Distortion Theory -- Models of the Near-Surface Distortions -- Models of Deep Geoelectric Structures -- Models of Deep Faults -- Interpretation of Magnetotelluric and Magnetovariational Data -- Statement of Inverse Problem -- The Interpretation Model -- Inversion Strategy.
520			_aMagnetotelluric methods are finding increasing applications for imaging electrically conductive structures below the Earth`s surface in both industrial and academic research. In Models and Methods of Magnetotellurics, the authors provide a systematic approach to understanding the modern theory of ill-posed problems which is essential to making confident meaningful interpretation of magnetotelluric and magnetovariational soundings. The interpretation is conducted out in an interactive way, including the hypotheses tests and successive partial inversions with priority of the tippers, magnetic tensors and impedance-phases, which keeps out the destructive static effects of near-surface inhomogeneities. The efficiency of the interpretation is exemplified by new geoelectric models of the Baikal rift zone and the Cascadian subduction zone.
650		0	_aEarth sciences.
650		0	_aGeology.
650		0	_aStructural geology.
650		0	_aGeophysics.
650		0	_aMagnetism.
650		0	_aMagnetic materials.
650	1	4	_aEarth Sciences.
650	2	4	_aGeophysics/Geodesy.
650	2	4	_aGeology.
650	2	4	_aEarth Sciences, general.
650	2	4	_aStructural Geology.
650	2	4	_aMagnetism, Magnetic Materials.
700	1		_aDmitriev, Vladimir I. _eauthor.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9783540778110
856	4	0	_uhttp://dx.doi.org/10.1007/978-3-540-77814-1
912			_aZDB-2-EES
950			_aEarth and Environmental Science (Springer-11646)
999			_c505880 _d505880