The Uryakh ore field (NE Transbaikalia): Formation of structural assemblages in the centroid-type seismic regime


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Abstract

Syn-ore centroid type deformations that produced unusual structural assemblages are identified in the Uryakh ore field. The regularities of the deformation process comparable to a mechanism of the centroid-type seismic focus are established. The results of studying fluid inclusions suggest that the pressure—temperature parameters of the system correspond to conditions typical of the seismic regime. A model of formation of structural assemblages in a centroid-type dynamic regime with the participation of fluids is proposed for the first time.

About the authors

T. M. Zlobina

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Author for correspondence.
Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

V. A. Petrov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

V. Yu. Prokofiev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

A. A. Kotov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

K. Yu. Murashov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

A. A. Wolfson

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tatiana1946@yandex.ru
Russian Federation, Staromonetny per. 35, Moscow, 119017

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