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STRUCTURE OF QUARTZ-VEIN ZONES IN SOUTH MUYA BLOCK OF THE WESTERN TRANSBAIKALIA
Abstract
Were described a quartz-veins zones which localized within metamorphosed rock of South Muya block Northeast part of Western Transbaikalia. During the research was received structural and material characteristics quartz veins different orientation of the creeks an Otvesny, a Krivoy and a Bambukoy river. Based of kinematic analysis, crack paragenesis highlighted and genetic nature is determined structural deformations. Thus was found out that paragenesis of quartz veins which has been studied was educated as a result of development deformations of thrust fault and left-side shear. Quartz-veins zones of creek Otvesny controlled by revers faults of the northwestern direction and meridional high-angled normal fault associated with the active development of the system of thrust. The development of quartz veins of the Kryvoy zone is associated with the structures formed in the later stages of the development of the thrust system. Within the Beregovay zone (Bambukoy river) quartz veins controlled by violations of the reverse-thrust and left later strike-slip nature.
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References13
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