Zobrazeno 1 - 5
of 5
pro vyhledávání: '"G. D. J. Sivakumar Sinha"'
Publikováno v:
Tectonophysics. 212:163-172
Aeromagnetic data over an 80-km-wide belt along the ENE-trending Narmada-Son lineament (NSL), starting from Baroda in the west and continuing to the south of Jabalpur in the east, has been studied to understand the structural and tectonic framework o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8bde90a00b67ebd8f315d81441356d8
https://doi.org/10.1016/0040-1951(92)90148-y
https://doi.org/10.1016/0040-1951(92)90148-y
Publikováno v:
Pure and Applied Geophysics PAGEOPH. 120:365-374
The self-potential anomaly due to a two-dimensional inclined sheets of finite depth extent has been analysed in the frequency domain using the Fourier transform. Expression for the Fourier amplitude and phase spectra are derived. The Fourier amplitud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::865e1558e256c63ac7a7ad9c90ffefd8
https://doi.org/10.1007/bf00877042
https://doi.org/10.1007/bf00877042
Publikováno v:
Journal of Earth System Science. 95:331-341
The magnetic anomaly over a two-dimensional thin horizontal plate is similar to the first horizontal derivative of the magnetic anomaly over a thick dipping dike of infinite depth extent but with a different direction of magnetization. Hence, the mag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9c6c7a6282fe2bce99aff45ca77d532
https://doi.org/10.1007/bf02842500
https://doi.org/10.1007/bf02842500
Publikováno v:
Exploration Geophysics. 13:5-9
An expression for the total field magnetic anomaly due to a two-dimensional prismatic body of finite depth extent is formulated and its Fourier transform is derived. Properties of the Fourier energy density and phase spectra are related to the body p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e71375dae4d5825dae84e146d45943ec
https://doi.org/10.1071/eg982005
https://doi.org/10.1071/eg982005
Publikováno v:
Journal of Earth System Science. 94:71-76
Expressions are derived for the horizontal and vertical gradients of the gravity anomaly over a thin dipping sheet of infinite depth extent. The resultant of these two gradients, known as the complex gradient, is also derived and properties of the am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8cdc219f641e5828d481e7279603874
https://doi.org/10.1007/bf02863410
https://doi.org/10.1007/bf02863410