Anisotropic transformation of the gravimetric field during tracing of discontinuous dislocations
Authors:
About authors
- North Caucasus State Technical University
Abstract
The traditional version of tracing discontinuous dislocations on the materials of gravity reconnaissance involves the transformation of the anomalous field into a field of complete horizontal gradient. In the presence of a complex, differently oriented fault system, the integral nature of the gravity field significantly complicates the solution of the problem. For such geological conditions, the anisotropic transformation method, which is characterized by greater efficiency and resolution, is proposed. The main characteristics of anisotropic transformation and recommendations on the choice of optimal transformation parameters are given.
Область исследования:
Geology
Funding:
None
Similar articles
Capillary forces as the main factor of oil displacement resistance in West Siberian fields
2003 E. Yu. Bolshakova
Material composition and formation conditions of Sarmatian deposits of the Stavropol arch
2003 A. V. Korkoshko