Please use this identifier to cite or link to this item:
https://hdl.handle.net/10216/52664Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.creator | A. Dória | |
| dc.creator | P. Morais | |
| dc.creator | M. Santos | |
| dc.creator | C. R. Gomes | |
| dc.creator | F. Noronha | |
| dc.creator | H. Sant'Ovaia | |
| dc.date.accessioned | 2022-09-08T11:59:16Z | - |
| dc.date.available | 2022-09-08T11:59:16Z | - |
| dc.date.issued | 2010 | |
| dc.identifier.other | sigarra:48377 | |
| dc.identifier.uri | https://hdl.handle.net/10216/52664 | - |
| dc.description.abstract | The main objective of this study was to determine the geometry of the FIP, in the Castelo Branco granite massif. This study showed that in addition to FIP in Mode I, are also present Mode II, suggesting that the directions found NE-SW to NNE-SSW and E-W to ESE-WNW can be interpreted as related to a maximum stress (σ1) oriented NE-SW. The NNW-SSE orientation corresponds to a late system | |
| dc.language.iso | por | |
| dc.rights | openAccess | |
| dc.rights.uri | https://creativecommons.org/licenses/by-nc/4.0/ | |
| dc.subject | Ciências da terra e ciências do ambiente | |
| dc.subject | Earth and related Environmental sciences | |
| dc.title | Estudo da microfracturação do maciço granítico de Castelo Branco através dos Planos de Inclusões Fluidas | |
| dc.type | Artigo em Revista Científica Nacional | |
| dc.contributor.uporto | Faculdade de Ciências | |
| dc.subject.fos | Ciências exactas e naturais::Ciências da terra e ciências do ambiente | |
| dc.subject.fos | Natural sciences::Earth and related Environmental sciences | |
| Appears in Collections: | FCUP - Artigo em Revista Científica Nacional | |
This item is licensed under a Creative Commons License
