INVERSION OF GRAVITY PROFILES BY USE OF A BACKUS‐GILBERT APPROACH
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Geophysical inversion methods are most effective when applied to linear functionals: it is therefore advantageous to employ linear models for geophysical data. A two‐dimensional linear model consisting of many horizontal prisms has been developed for interpretation of gravity profiles. A Backus‐Gilbert inversion which finds the acceptable model “nearest” to an initial estimate can be rapidly computed; iterative application of the technique allows a single‐density model to be developed at a modest expense in computer time. Gravity data from the Guichon Creek batholith were inverted as a test of the method, with results comparable to those from a standard polygon model.
2004 ◽
Vol 61
(1)
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pp. 134-146
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2021 ◽
Vol 6
(3)
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pp. 26
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2021 ◽
Vol 20
(1)
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pp. 1-23
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2020 ◽
Vol 6
(5)
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pp. 21-25
2016 ◽
Vol 23
(1)
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pp. 3-42
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