Tectogenesis of the Krivoy Rog structure according to the results of interpretation of magnetometric data obtained in the superdeep well
© Kovalenko-Zavoyskiy V.N., Ivashchenko I.N.
Based upon the studies of anisotropy of magnetic susceptibility of the core of the Krivoy Rog superdeep well and interpretation of anomalous magnetic field of the well the conclusion has been made that the Western Fold is not the core of the Krivoy Rog synclinorium but is thrusted over the saksagan suite, while the last one sunk under it due to the excess weight during the stage of Proterozoic remobilization of the Archean ingulets plagiogranites. <<back |
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