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


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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.

作者简介

T. Zlobina

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

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Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

V. Petrov

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

Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

V. Prokofiev

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

Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

A. Kotov

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

Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

K. Murashov

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

Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

A. Wolfson

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

Email: tatiana1946@yandex.ru
俄罗斯联邦, Staromonetny per. 35, Moscow, 119017

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