Gravity modelling of an interface above which the density contrast decreases hyperbolically with depth

dc.contributor.author Visweswara Rao, C.
dc.contributor.author Raju, M. L.
dc.contributor.author Chakravarthi, V.
dc.date.accessioned 2022-03-26T23:50:14Z
dc.date.available 2022-03-26T23:50:14Z
dc.date.issued 1995-01-01
dc.description.abstract An interpretational procedure for determining the depth of an interface underlying sediments whose density contrast decreases hyperbolically with depth is developed. The approximate depth of the interface at each gravity station is calculated by using the gravity formula of an infinite slab with a hyperbolic density contrast. Based on these depth values, the sediment-basement interface is replaced by an n-sided polygon. Its gravity anomaly is computed by using the formula of Visweswara Rao et al. (1994). These depth values are refined using the procedure of Bott (1960). © 1995.
dc.identifier.citation Journal of Applied Geophysics. v.34(1)
dc.identifier.issn 09269851
dc.identifier.uri 10.1016/0926-9851(94)00057-U
dc.identifier.uri https://www.sciencedirect.com/science/article/abs/pii/092698519400057U
dc.identifier.uri https://dspace.uohyd.ac.in/handle/1/2670
dc.title Gravity modelling of an interface above which the density contrast decreases hyperbolically with depth
dc.type Journal. Article
dspace.entity.type
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