### Abstract

The Hilbert Transform of the second order horizontal gradient of the gravity effect of a two dimensional dipping fault is derived. Using the derivatives of the horizontal gradient of the gravity effect and the Hilbert Transform, the parameters of the dipping fault, namely the dip, the depths to the top and bottom and the density contrast, are obtained. The gravity effect of the vertical fault has also been analysed treating it as a particular case of the dipping fault.-from Authors

Original language | English |
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Title of host publication | Journal of Geophysics - Zeitschrift fur Geophysik |

Pages | 34-41 |

Number of pages | 8 |

Volume | 53 |

Edition | 1 |

Publication status | Published - 1983 |

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### ASJC Scopus subject areas

- Earth and Planetary Sciences(all)
- Environmental Science(all)

### Cite this

*Journal of Geophysics - Zeitschrift fur Geophysik*(1 ed., Vol. 53, pp. 34-41)

**Gravity interpretation of two dimensional fault structures using Hilbert transforms.** / Sundararajan, N.; Mohan, N. L.; Seshagiri Rao, S. V.

Research output: Chapter in Book/Report/Conference proceeding › Chapter

*Journal of Geophysics - Zeitschrift fur Geophysik.*1 edn, vol. 53, pp. 34-41.

}

TY - CHAP

T1 - Gravity interpretation of two dimensional fault structures using Hilbert transforms.

AU - Sundararajan, N.

AU - Mohan, N. L.

AU - Seshagiri Rao, S. V.

PY - 1983

Y1 - 1983

N2 - The Hilbert Transform of the second order horizontal gradient of the gravity effect of a two dimensional dipping fault is derived. Using the derivatives of the horizontal gradient of the gravity effect and the Hilbert Transform, the parameters of the dipping fault, namely the dip, the depths to the top and bottom and the density contrast, are obtained. The gravity effect of the vertical fault has also been analysed treating it as a particular case of the dipping fault.-from Authors

AB - The Hilbert Transform of the second order horizontal gradient of the gravity effect of a two dimensional dipping fault is derived. Using the derivatives of the horizontal gradient of the gravity effect and the Hilbert Transform, the parameters of the dipping fault, namely the dip, the depths to the top and bottom and the density contrast, are obtained. The gravity effect of the vertical fault has also been analysed treating it as a particular case of the dipping fault.-from Authors

UR - http://www.scopus.com/inward/record.url?scp=0021035662&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0021035662&partnerID=8YFLogxK

M3 - Chapter

AN - SCOPUS:0021035662

VL - 53

SP - 34

EP - 41

BT - Journal of Geophysics - Zeitschrift fur Geophysik

ER -