Writers : Ardestani.V. E
Refference : Geosciences Scientific Quarterly Journal,No.:47-48,P.:123
Publishing Year : 1382

Abstract :
Euler's homogeneity equation for determining the coordinates of the source body especially to estimate the depth (EULDPH) is discussed at this paper. This method is applied to synthetic and high-repolution real data such as gradiometiic or microgravity data Low-quality gravity data especially in the areas with a complex geology structure has rarely been used. The Bouguer gravity anomalies are computed from absolute gravity data after the required corrections Bouguer anomaly is transferred to residual gravity anomaly. The gravity gradients are estimated from residual anomaly values. Then by applying the gravity gradients, using EULDPH, the coordinates of the perturbiug body will be determined. Two field examples one in the east of Tehran (Mard Abad) where we would like to determine the location of the anomaly (hydrocarbon) and another in the south-east of Iran close to the border with Mghanestan (Nosrat Abad) where we are exploring choromit are presented.
Subject List : gravimetry