These techniques have varying complexity in the interpretation.Īll different simple models may not be found in real subsurface geological situations, they usually are preferred in practical inversion of many isolated sources. Analytical formula for basic geometrical shapes and many approaches have been produced to translate the gravity anomaly expecting the body of basic geometry (sphere, horizontal cylinder and vertical cylinder). Understanding of gravity data can be performed utilizing basic geometrical models, forward modeling and inversion. To overcome these issues, we find a preferred geometry to subsurface structures with a known density followed by the inversion processes. Clarification of gravity data is constantly connected with the ill-posed and non-unique problems. The main objective of the gravity interpretation is evaluating the model parameters (depth, amplitude coefficient, origin location, and shape parameter) of gravity oddities delivered by basic geometrical formed structures (spheres, cylinders). It has much beneficial utilization in hydrocarbon exploration, mineral prospecting, archeological investigations, environmental applications and crustal imaging. Gravity method is a non-ruinous geophysical procedure that measures contrasts in the gravitational field of the earth at many various areas.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |