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ROTATION OF CRUSTAL BLOCKS BETWEEN SHEAR ZONES IN LOWER PRIAMURYE, ACCORDING TO MORPHOSTRUCTURAL DATA

https://doi.org/10.15356/0435-4281-2017-4-64-75

Abstract

The Lower Priamurye geoblock (the first-rank structural element of the Amur plate) was distinguished based on the morphostructural data. This geoblock is affected by neotectonic right-lateral strike-slip displacements along northeast-striking transregional faults. Arc faults have been formed inside the geoblock due to the imposed stresses. The faults are geomorphologically expressed as a conjugate system of river valleys bordering four blocks with rounded habitus that are composed of Mesozoic-Cenozoic magmatic and folded sedimentary rocks. A vortex-like arrangement of the faults inside the blocks, and the right-lateral strike-slip displacements consistent with the direction of deformations along the northeast striking faults, indicate the counter-clockwise rotation of these blocks.

About the Authors

F. S. Onukhov
Kosygin Institute of Tectonics and Geophysics FEB RAS
Russian Federation
Khabarovsk


T. V. Merkulov
Kosygin Institute of Tectonics and Geophysics FEB RAS
Russian Federation
Khabarovsk


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Review

For citations:


Onukhov F.S., Merkulov T.V. ROTATION OF CRUSTAL BLOCKS BETWEEN SHEAR ZONES IN LOWER PRIAMURYE, ACCORDING TO MORPHOSTRUCTURAL DATA. Geomorfologiya. 2017;(4):64-75. (In Russ.) https://doi.org/10.15356/0435-4281-2017-4-64-75

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