@article{Sokolov_2017,<br/><span class="tab"></span>
	doi = {10.5800/gt-2017-8-4-0316},<br/><span class="tab"></span>
	url = {https://doi.org/10.5800%2Fgt-2017-8-4-0316},<br/><span class="tab"></span>
	year = 2017,<br/><span class="tab"></span>
	month = {jan},<br/><span class="tab"></span>
	publisher = {Institute of Earth{\textquotesingle}s Crust,<br/><span class="tab"></span> Siberian Branch of the Russian Academy of Sciences},<br/><span class="tab"></span>
	volume = {8},<br/><span class="tab"></span>
	number = {4},<br/><span class="tab"></span>
	pages = {769--789},<br/><span class="tab"></span>
	author = {S. Yu. Sokolov and A. S. Abramova and E. A. Moroz and Yu. A. Zaraiskaya},<br/><span class="tab"></span>
	title = {{AMPLITUDES} {OF} {DISJUNCTIVE} {DISLOCATIONS} {IN} {THE} {KNIPOVICH} {RIDGE} {FLANKS} ({NORTHERN} {ATLANTIC}) {AS} {AN} {INDICATOR} {OF} {MODERN} {REGIONAL} {GEODYNAMICS}},<br/><span class="tab"></span>
	journal = {Geodynamics {\&}amp$\mathsemicolon$ Tectonophysics}
<br/>}