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Index Geophysics

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
 

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