000			03332nam a22005175i 4500
001			978-94-007-0406-0
003			DE-He213
005			20140220083337.0
007			cr nn 008mamaa
008			120303s2012 ne | s |||| 0|eng d
020			_a9789400704060 _9978-94-007-0406-0
024	7		_a10.1007/978-94-007-0406-0 _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		_aMallick, K. _eauthor.
245	1	0	_aBouguer Gravity Regional and Residual Separation: Application to Geology and Environment _h[electronic resource] / _cby K. Mallick, A. Vasanthi, K. K. Sharma.
264		1	_aDordrecht : _bSpringer Netherlands, _c2012.
300			_aX, 250p. 70 illus., 10 illus. in color. _bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_aonline resource _bcr _2rdacarrier
347			_atext file _bPDF _2rda
505	0		_aPreface -- 1. Introduction -- 2. Regional and residual gravity anomalies : The existing issues -- 3. New computational schemes -- 4. Applications to geological and environmental problems -- 5. Hydrocarbon -- 6. Minerals and Groundwater -- 7. Structural studies -- 8. Isostatic studies -- 9. Vertical Crustal Movements -- 10. Engineering Applications and earthquake studies -- 11. Other applications -- Index.
520			_aThe process of regional-residual separation in potential field is age-old.  Broadly, there are two techniques for regional-residual resolution, viz., graphical and analytical. Both the techniques have their own respective shortcomings. In this book, the authors have described the technique based on finite element method in which only eight (or twelve) nodal observed gravity values are used for the regional computation, thereby eliminating the possible contamination of anomalous fields and also the technique does not assume an explicit model and physical properties like density of rocks etc. in the regional computation. The book discusses the advantages of this technique viz., it is not site-specific; the computation is independent of any prior assumptions as to the form and depth of shallow or deeper structures; it can handle data distributed at random or on a regular grid on the map space; and the neighbouring surveys join smoothly.   The book focuses on application of this new technique which has been demonstrated in different fields, such as hydrocarbon, minerals and groundwater, structural studies, earthquake and engineering studies and impact structures.
650		0	_aGeography.
650		0	_aPhysical geography.
650		0	_aMines and mineral resources.
650		0	_aEngineering.
650	1	4	_aEarth Sciences.
650	2	4	_aGeophysics/Geodesy.
650	2	4	_aGeotechnical Engineering & Applied Earth Sciences.
650	2	4	_aEngineering, general.
650	2	4	_aMineral Resources.
650	2	4	_aMeasurement Science and Instrumentation.
700	1		_aVasanthi, A. _eauthor.
700	1		_aSharma, K. K. _eauthor.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9789400704053
856	4	0	_uhttp://dx.doi.org/10.1007/978-94-007-0406-0
912			_aZDB-2-EES
999			_c104274 _d104274