On the stress tensor in Vrancea region
Item
Title (Dublin Core)
en-US
On the stress tensor in Vrancea region
Description (Dublin Core)
en-US
Presented is a new application of Gephart-Forsyth inverse technique for predicting directions and senses of slip. In Vrancea region, the compression axis is thus found to act in a NE-SW direction and not in a SE-NW direction, as is commonly thought from focal mechanism results. In addition, evidence is provided that the stresses in the crust are decoupled from those in the subducted slab.
ARK: https://n2t.net/ark:/88439/y054021
Permalink: https://geophysicsjournal.com/article/101
ARK: https://n2t.net/ark:/88439/y054021
Permalink: https://geophysicsjournal.com/article/101
Creator (Dublin Core)
Oncescu, M.C.
Subject (Dublin Core)
en-US
Stress tensor
en-US
Vrancea region
en-US
Geodynamics
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1987-11-05
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/101
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 62 No 1 (1988): Journal of Geophysics; 62-65
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/101/63