Abstract
The article presents the new data concerning the bounding zones of the Archean - Early Proterozoic Taratash block. It breaks the longitude structure of the Urals, squeezing all structural zones at a latitude of the town Miass. There were studied the meso- and microstructures of the boundary zones, anisotropy of magnetic susceptibility of faulted rocks and distribution of seismic waves velocities in to blastomylonites. We suggest that kinematic history of the Taratash block consists of two phases: 1) Middle Riphean exhumation of Taratash rocks in tension environ- ment; 2) Late Paleozoic formation of Indenter due regional shortening setting.
Highlights
The article presents the new data concerning the bounding zones of the Archean — Early Proterozoic Taratash block
We suggest that kinematic history of the Taratash block consists of two phases: 1) Middle Riphean exhumation of Taratash rocks in tension environment; 2) Late Paleozoic formation of Indenter due regional shortening setting
Бельдишско-Куватальская зона тектонитов, первоначально маркировавшая более или менее прямолинейный пологий сброс, была деформирована (изогнута) и превратилась в зону надвига, расположенного во фронтальной части Тараташского индентора
Summary
The article presents the new data concerning the bounding zones of the Archean — Early Proterozoic Taratash block. Микроструктуры тектонитов, анизотропия магнитной восприимчивости и скорости прохождения сейсмических волн в бластомилонитах. По положению в структуре выделены три главные зоны распространения тектонитов бельдишского комплекса Для изучения состава и физических свойств бластомилонитов были отобраны пробы из керна скважин 311, 319 и 323
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
