GRAVITY INTERPRETATION VIA EULDPH

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E.ARDESTANI V.

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Journal Paper

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Journal: GEOSCIENCES Year:2003 | Volume:11 | Issue:47-48 Page(s): 123-118

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Information Journal Paper

Title

GRAVITY INTERPRETATION VIA EULDPH

Author(s)

E.ARDESTANI V.

Keywords

BOUGUER ANOMALY

RESIDUAL ANOMALY

GRAVITY GRADIENT

EULDPH

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-resolution real data such as gradiometric 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 perturbing 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 Afghanestan (Nosrat Abad) where we are exploring choromit are presented.

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APA: Copy

E.ARDESTANI, V.. (2003). GRAVITY INTERPRETATION VIA EULDPH. GEOSCIENCES, 11(47-48), 123-118. SID. https://sid.ir/paper/528507/en

Vancouver: Copy

E.ARDESTANI V.. GRAVITY INTERPRETATION VIA EULDPH. GEOSCIENCES[Internet]. 2003;11(47-48):123-118. Available from: https://sid.ir/paper/528507/en

IEEE: Copy

V. E.ARDESTANI, “GRAVITY INTERPRETATION VIA EULDPH,” GEOSCIENCES, vol. 11, no. 47-48, pp. 123–118, 2003, [Online]. Available: https://sid.ir/paper/528507/en

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