| 1. | Also these changes can be presented as gravity anomaly temporal variations.
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| 2. | Above we already made use of " gravity anomalies " \ Delta g.
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| 3. | Or it might just be a merge into Gravity anomaly.
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| 4. | Some corrections that are needed for gravity anomalies are less important for magnetic anomalies.
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| 5. | For even closer trajectories, gravity anomalies may be important.
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| 6. | See Gravity anomaly, Physical geodesy talk ) 12 : 53, 23 April 2010 ( UTC)
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| 7. | This shear zone is associated with one of the largest gravity anomalies known from continental interiors.
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| 8. | As such, gravity anomalies describe the local variations of the gravity field around the model field.
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| 9. | The FTFZ is flanked by two negative gravity anomalies associated with the accretion of igneous crust.
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| 10. | Inversion of strong negative isostatic gravity anomalies in confined deep basins caused by upper crustal stretching.
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