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Books > Earth & environment > Geography > Cartography, geodesy & geographic information systems (GIS) > Map making & projections
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Quantification of Gravity Anomalies for Subsurface Geological Structures using Variable Density Contrast - Algorithms and Computer Programs (Hardcover, 1st ed. 2020)
Loot Price: R2,882
Discovery Miles 28 820
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Quantification of Gravity Anomalies for Subsurface Geological Structures using Variable Density Contrast - Algorithms and Computer Programs (Hardcover, 1st ed. 2020)
Series: Lecture Notes in Earth System Sciences
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Computer based algorithms to analyze gravity anomalies for
subsurface structures have gained momentum in the search of natural
resources. The enormous progress since then, however, led to the
development of new interpretational techniques with increasing
accuracy to analyze the gravity anomalies. The fact that variable
density models yield more reliable interpretations has paved the
way for developing new analytical tools to analyze gravity
anomalies. In this book, the parabolic density function which
unambiguously describes the density-depth dependence of sedimentary
rocks is used to design new algorithms and relevant GUI based JAVA
programs to analyze the gravity anomalies of subsurface geological
structures. Although the terms modeling and inversion are used more
or less synonymously to refer to various interpretation strategies
of gravity anomalies, criteria has been formulated and followed to
design modeling and inversion strategies of gravity anomalies.
Accordingly, automatic inversion algorithms coupled with relevant
computer codes to analyze the gravity anomalies due to 2-D and
2.5-D fault structures described with both planar and non-planar
fault planes are presented. Automatic techniques based on modeling
and inversion principles to analyze the gravity anomalies due to
2-D and 2.5-D sedimentary basins even when the profile of
interpretation fails to bisects the strike length of the target are
presented with related software. Automatic modeling and inversion
techniques for the analysis of measured gravity anomalies due to
3-D sedimentary basins are presented. Also new is the automatic
determination of regional gravity background in case of inversion
algorithms. The highlight of the book is that, in each case, the
robustness is demonstrated with both synthetic and real field
gravity anomalies. Thus this book is very useful to academicians,
researchers and field geophysicists.
To the best of my knowledge no comprehensive book is available to
address the issues described above and hence this volume would
certainly attract the market.
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