Gravity anomalies of strike limited listric fault sources with analytically defined fault planes and arbitrary density contrast variations with depth

References

1. AbdelrahmanE.S.M., El‐ArabyH.M., El‐ArabyT.M. and Abo‐EzzE.R.2003. A least‐squares derivatives analysis of gravity anomalies due to faulted thin slabs. Geophysics68, 535–543.
   [Google Scholar]
2. ChaiY. and HinzeW.J.1988. Gravity inversion of an interface above which the density contrast varies exponentially with depth. Geophysics53, 837–845.
   [Google Scholar]
3. ChakravarthiV.2009. Gravity anomalies of pull‐apart basins having finite strike length with depth dependent density: A ridge regression inversion. Near Surface Geophysics7, 217–226.
   [Google Scholar]
4. ChakravarthiV. and SundararajanN.2004. Ridge regression algorithm for gravity inversion of fault structures with variable density. Geophysics69, 1394–1404.
   [Google Scholar]
5. ChakravarthiV. and Sundararajan, N.2007. 3D gravity inversion of basement relief – A depth dependent density approach. Geophysics72, I23–I32.
   [Google Scholar]
6. ChappelA. and KusznirN.2008. An algorithm to calculate the gravity anomaly of sedimentary basins with exponential density‐depth relationships. Geophysical Prospecting56, 249–258.
   [Google Scholar]
7. CordellL.1973. Gravity anomalies using an exponential density‐depth function – San Jacinto Graben, California. Geophysics38, 684–690.
   [Google Scholar]
8. DixitM.M., Satya VaniN., SarkarD., KhareP. and ReddyP.R.2000. Velocity inversion in the Lodhika area, Saurashtra peninsula, Western India. First Break18, 499–504.
   [Google Scholar]
9. Gallardo‐DelgadoL.A., Perez‐Flores, M.A. and Gomez‐TrevinoE.2003. A versatile algorithm for joint inversion of gravity and magnetic data. Geophysics68, 949–959.
   [Google Scholar]
10. García‐AbdeslemJ.2000. 2‐D inversion of gravity data using sources laterally bounded by continuous surfaces and depth‐dependent density. Geophysics65, 1128–1141.
    [Google Scholar]
11. García‐AbdeslemJ.2003. 2D modeling and inversion of gravity data using density contrast varying with depth and source‐basement geometry described by the Fourier series. Geophysics68, 1909–1916.
    [Google Scholar]
12. García‐AbdeslemJ.2005. The gravitational attraction of a right rectangular prism with density varying with depth following a cubic polynomial. Geophysics70, J39–J42.
    [Google Scholar]
13. GeldartL.P., GillD.E. and SharmaB.1966. Gravity anomalies of two‐dimensional faults. Geophysics31, 372–397.
    [Google Scholar]
14. GoussevS., ChartersR. and PeirceJ.2006. Mackenzie Delta: A case of one residual gravity anomaly and 16 dry exploration wells. 2006 CSPG/CSEG/CWLS Joint Conference, 15–18 May, Calgary, Canada, Expanded Abstracts, 435–439.
    [Google Scholar]
15. JacksonJ.A.1987. Active normal faulting and crustal extension. Geological Society, London, Special Publications28, 3–17. doi:10.1144/GSL.SP.1987.028.01.02
    [Google Scholar]
16. LitinskyV.A.1989. Concept of effective density: Key to gravity depth determinations for sedimentary basins. Geophysics54, 1474–1482.
    [Google Scholar]
17. Martín AtienzaB. and García‐AbdeslemJ.1999. 2‐D gravity modeling with analytically defined geometry and quadratic polynomial density functions. Geophysics64, 1730–1734.
    [Google Scholar]
18. MurthyI.V.R.1998. Gravity and Magnetic Interpretation in Exploration Geophysics.Geological Society of India.
    [Google Scholar]
19. MurthyI.V.R. and RaoD.B.1980. Interpretation of gravity anomalies over faults and dykes by Fourier transforms, employing end correction. Geophysical Research Bulletin18, 95–110.
    [Google Scholar]
20. PaulM.K., DuttaS. and BanerjeeB.1966. Direct interpretation of two dimensional structural faults from gravity data. Geophysics31, 940–948.
    [Google Scholar]
21. PeirceJ.W. and LipkovL.1988. Structural interpretation of the Rukwa Rift, Tanzania. Geophysics53, 824–836.
    [Google Scholar]
22. PrietoC., PerkinsC. and BerkmanE.1985. Columbia River Basalt plateau: An integrated approach to interpretation of basalt‐covered areas. Geophysics50, 2709–2719.
    [Google Scholar]
23. RaoD.B.1985. Analysis of gravity anomalies over an inclined fault with quadratic density function. Pure and Applied Geophysics123, 250–260.
    [Google Scholar]
24. RaoC.V., PramanikAG., KumarG.V.R.K. and RajuM.L.1994. Gravity interpretation of sedimentary basins with hyperbolic density contrast. Geophysical Prospecting42, 825–839
    [Google Scholar]
25. SariC. and SalkM.2002Analysis of gravity anomalies with hyperbolic density contrast: An application to the gravity data of Western Anatolia. Journal of Balkan Geophysical Society5, 87–96.
    [Google Scholar]
26. SundararajanN. and BrahmamG.R.1998. Spectral analysis of gravity anomalies caused by slab‐like structures: A Hartley transform technique. Journal of Applied Geophysics39, 53–61.
    [Google Scholar]
27. SundararajanN., MohanN.L. and RaoS.V.S.1983. Gravity interpretation of 2D fault structures using Hilbert transforms. Journal of Geophysics53, 34–41.
    [Google Scholar]
28. TorizinJ., JentzschG., MalischewskyP., KleyJ., AbakanovN. and KurskeevA.2009. Rating of seismicity and reconstruction of the fault geometries in northern Tien Shan within the project “Seismic Hazard Assessment for Almaty”. Journal of Geodynamics48, 269–278.
    [Google Scholar]
29. ZhangJ., ZhongB., ZhouX. and DaiY.2001, Gravity anomalies of 2‐D bodies with variable density contrast. Geophysics66, 809–813.
    [Google Scholar]
30. ZhouX.2008. Two‐dimensional (2D) vector gravity potential and general line integrals for gravity anomaly due to 2D masses of depth‐dependent density contrast. Geophysics73, I43–I50.
    [Google Scholar]
31. ZhouX.2009. General line integrals for gravity anomalies of irregular two‐dimensional (2D) masses with horizontally‐ and vertically‐dependent density contrast. Geophysics74, I1–I7.
    [Google Scholar]