The hercynian imposed deformations in the Golets Vysochaishii deposit structure (Baikal-Patom belt), <sup>40</sup>Ar/<sup>39</sup>Ar data

Author:

Vanin V. A.1,Mazukabzov A. M.1,Yudin D. S.2,Blinov A. V.3,Tarasova Yu. I.3

Affiliation:

1. Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences

2. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

3. Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences

Abstract

The paper presents the results of the detailed structural analysis and 40Ar/39Ar dating of the deformations in the Golets Vysochaishii deposit area. The geological and structural studies showed the folded-deformation sequence from large lying folds through axial-plane cleavage formation and cleavage to quartz-filled fractures. The 40Ar/39Ar dating of syntectonic sericite yielded the ages of two Hercynian tectonic impulses – 340 and 320 Ma. This stage is characterized by the earlier-known successive complication of the Early Paleozoic fold-nappe structure of the area. Analysis has been made on four samples taken from different sites and characterized by different sets of deformational structures. The 40Ar/39Ar age of 340 Ma reflects the formation of small-size folds as a result of interlayer sliding and sliding along the cleavage axial planes. The 40Ar/39Ar age of 320 Ma reflects the formation of discretely manifested crenulation cleavage and low-Au, low-sulfidation quartz veins oriented obliquely to the elements of bedding and axial-plane cleavage.

Publisher

Institute of Earth's Crust, Siberian Branch of the Russian Academy of Sciences

Subject

Earth-Surface Processes,Geophysics

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