| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4701485 | Earth Science Frontiers | 2009 | 8 Pages |
Abstract
Results of data processing of marine magnetic surveys in a southern part of Barents Sea, executed from 1986 to 2001 are considered. The geomagnetic investigation of Southern Barents Sea bottom points on its complicated many-stage geologic-tectonic structures in which two disjunctive structures prevail: Riphean-Vendian inherited rift structures with north-west strike and orthogonal system of superposed faults transformed in north-eastern direction. Late Devonian alkaline intrusives with associated ore mineralization are confined to points of these systems intersection.
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