DIRECT INTERPRETATION OF TWO‐DIMENSIONAL STRUCTURAL FAULTS FROM GRAVITY DATA
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Some methods of direct determination of the parameters of a two‐dimensional structural fault with horizontal plane faces, from the gravity profile caused by it, have been formulated in this paper. The upward continuation of the two‐dimensional gravity profile plays an important role in these methods. The determinations by these methods are unique for structures of the same type in the sense that no structure of the same type other than that arrived at by the proposed methods can give rise to the observed anomaly. The necessary coefficients for upward continuation of two‐dimensional gravity data and the theory involved in their determinations form the appendix of this paper.
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1981 ◽
Vol GE-19
(4)
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pp. 194-203
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1948 ◽
Vol 39
(299)
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pp. 992-1001
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1945 ◽
Vol 36
(252)
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pp. 66-72
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