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Detection of High-Potential Oil and Gas Fields Using Normalized Full Gradient of Gravity Anomalies: A Case Study in the Tabas Basin, Eastern Iran

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Abstract

The normalized full gradient (NFG) represents the full gradient of the gravity anomaly at a point divided by the average of the full gradient at the same point. The NFG minimum between two maxima in an NFG section or a closed minimum surrounded by closed maxima on an NFG map may indicate density-deficient anomalies closely related to possible oil–gas reservoirs. On a cross-section, closed minima can be used to estimate the depth to centers of possible hydrocarbon reservoirs. The NFG map can also be used to locate oil–gas exploratory wells for estimation of the depth of possible reservoirs. The objective of this paper is to use two and three-dimensional (2D and 3D) NFG on gravity data of the Tabas basin in Yazd province, eastern Iran. A hypothetical model is first considered to explore the NFG characteristics and their relationship with the geometry of the model. The physical properties of the model are then studied to simplify the interpretation of real data. Finally 2D and 3D NFG models are developed for real gravity data to predict the location of any possible high potential oil–gas reservoirs. The results obtained indicate two zones in the northern and central parts of the Tabas basin suitable for hydrocarbon prospecting. However, the favorable zone located in the middle of the basin in which anticline E is detected at a depth of 5–7 km is more important for the purpose of hydrocarbon exploration.

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Acknowledgments

We are most grateful for the support of the National Oil Company of Iran (NIOC), Special thanks to Mr. Khorasani and Dr. Tabatabei from the geophysics department of NIOC for providing the Tabas gravity data. We would also like to thank Dr. Dondurur for his helpful comments and suggestions.

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Correspondence to Hamid Aghajani.

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Aghajani, H., Moradzadeh, A. & Zeng, H. Detection of High-Potential Oil and Gas Fields Using Normalized Full Gradient of Gravity Anomalies: A Case Study in the Tabas Basin, Eastern Iran. Pure Appl. Geophys. 168, 1851–1863 (2011). https://doi.org/10.1007/s00024-010-0169-y

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