Tectonic Fracturing of the Lithosphere of the Priamurye Region by Submeridional and Sublatitudinal Faults (from Geophysical Data and Relief Analysis)
- Authors: Merkulova T.V.1, Gil’manova G.Z.1, Tusikova S.A.1
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Affiliations:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
- Issue: Vol 13, No 6 (2019)
- Pages: 510-521
- Section: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211718
- DOI: https://doi.org/10.1134/S181971401906006X
- ID: 211718
Cite item
Abstract
Based on the data of relief analysis, the gravity and magnetic anomaly axes, earthquake foci sequences, and Vp/Vs ratio values, tectonic fracturing of the lithosphere is studied and tectonic submeridionally and sublatitudinally oriented fracturing zones are distinguished in the Priamurye region. Separate segments of extended submeridional and sublatitudional fracturing zones are evidenced from the regional faults detected using the geological methods. Submeridionally oriented tectonic fracturing zones are mostly revealed, which do not correlate with the regional faults. Fracturing zones of similar orientation which are displayed in lineaments of different type and correlate with the seismoactive zones may be considered as hidden faults.
Keywords
About the authors
T. V. Merkulova
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Author for correspondence.
Email: merculova@itig.as.khb.ru
Russian Federation, Khabarovsk, 680000
G. Z. Gil’manova
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Email: merculova@itig.as.khb.ru
Russian Federation, Khabarovsk, 680000
S. A. Tusikova
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Email: merculova@itig.as.khb.ru
Russian Federation, Khabarovsk, 680000