POSSIBILITIES OF THE METHOD OF ANISOTROPY OF MAGNETIC SUSCEPTIBILITY IN THE SOLUTION OF GEOLOGIC-GEOPHYSICAL PROBLEMS OF SEARCH RADICAL DIAMOND FIELDS
Principal physics of a method of anisotropy of magnetic susceptibility (AMS) of rocks allows to use it in the solution of a wide range of geologic-geophysical tasks. In comparison with other methods of studying of a petrotexture of rocks the method of an AMS differs in a high precision, efficiency of obtaining results, unambiguity of interpretation and so forth. The experience got as a result of studying of AMS of various structural and real complexes of the Yakutia and Arkhangelsk kimberlite provinces allows to use a method by search of radical diamond fields and other minerals.