2025-02-23T08:43:31-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: Query fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22journalsuranua-geofizicheskiy-article-111028%22&qt=morelikethis&rows=5
2025-02-23T08:43:31-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: => GET http://localhost:8983/solr/biblio/select?fl=%2A&wt=json&json.nl=arrarr&q=id%3A%22journalsuranua-geofizicheskiy-article-111028%22&qt=morelikethis&rows=5
2025-02-23T08:43:31-05:00 DEBUG: VuFindSearch\Backend\Solr\Connector: <= 200 OK
2025-02-23T08:43:31-05:00 DEBUG: Deserialized SOLR response
Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea

Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea

It has been shown on the base of considerable tectonophysical material that producing of up-to-date tectonic disruptions within the limits of the Mountain Crimea is specified by broad spectrum of deformational regimes and kinematic environments. The technique of plotting is methodologically substant...

Full description

Saved in:
Bibliographic Details
Main Author: Vol'fman, Yu.M.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Subjects:
tectonic faulting
the stress fields
deformation modes
kinematic conditions
stereographic models
shifts
upthrusts
faults
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111028
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:It has been shown on the base of considerable tectonophysical material that producing of up-to-date tectonic disruptions within the limits of the Mountain Crimea is specified by broad spectrum of deformational regimes and kinematic environments. The technique of plotting is methodologically substantiated for stereographical models of deformational regimes by averaging the parameters of structural-kinematic parageneses of tectonic disruptions and displacements produced in similar conditions. These models reflect adequately regional environments of producing tectonic disruptions. Quantitative ratio of slickensides in parageneses, which make up the basis of corresponding models specify the measure of effects of these or other deformational regimes on the processes of tectogenesis in  the region. The models and examples of shearing, upthrust- and upthrust-displacement deformational regimes are presented and their description is given.

Similar Items