2013
DOI: 10.1134/s1028334x12110177
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The structural peculiarities of the Dzhetygara-Troitsk Zone, Southern Urals (Based on the URSEIS-95 profile)

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Cited by 3 publications
(2 citation statements)
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“…Some additional work has been done for a better understanding of the URSEIS profile as well. As was pointed out by Znamenskii et al (2013), the pattern of reflectors in the eastern part of the profile, to the east of Kartaly town and the Kartaly (Troitsk) regional fault, a typical flower structure is present, which supports and is evidence for the idea of a wide development of movement along strike-slip faults in this part of the Urals.…”
Section: Structural Researchsupporting
confidence: 72%
“…Some additional work has been done for a better understanding of the URSEIS profile as well. As was pointed out by Znamenskii et al (2013), the pattern of reflectors in the eastern part of the profile, to the east of Kartaly town and the Kartaly (Troitsk) regional fault, a typical flower structure is present, which supports and is evidence for the idea of a wide development of movement along strike-slip faults in this part of the Urals.…”
Section: Structural Researchsupporting
confidence: 72%
“…As was pointed out by Znamenskii et al (2013), the pattern of reflectors in the eastern part of the profile, to the east of Kartaly town and the Kartaly (Troitsk) regional fault, a typical flower structure is present, which supports and is evidence for the idea of a wide development of movement along strike-slip faults in this part of the Urals.…”
Section: Structural Researchsupporting
confidence: 57%