Dolomite microstructures between 390° and 700 °C: Indications for deformation mechanisms and grain size evolution
| Data(s) |
2016
|
|---|---|
| Formato |
application/pdf |
| Identificador |
http://boris.unibe.ch/83970/1/Bergeratal_JSG2016.pdf Berger, Alfons; Ebert, Andreas; Ramseyer, Karl; Gnos, Edwin; Decrouez, Danielle (2016). Dolomite microstructures between 390° and 700 °C: Indications for deformation mechanisms and grain size evolution. Journal of structural geology, 89, pp. 144-152. Pergamon 10.1016/j.jsg.2016.06.001 <http://dx.doi.org/10.1016/j.jsg.2016.06.001> doi:10.7892/boris.83970 info:doi:10.1016/j.jsg.2016.06.001 urn:issn:0191-8141 |
| Idioma(s) |
eng |
| Publicador |
Pergamon |
| Relação |
http://boris.unibe.ch/83970/ |
| Direitos |
info:eu-repo/semantics/restrictedAccess |
| Fonte |
Berger, Alfons; Ebert, Andreas; Ramseyer, Karl; Gnos, Edwin; Decrouez, Danielle (2016). Dolomite microstructures between 390° and 700 °C: Indications for deformation mechanisms and grain size evolution. Journal of structural geology, 89, pp. 144-152. Pergamon 10.1016/j.jsg.2016.06.001 <http://dx.doi.org/10.1016/j.jsg.2016.06.001> |
| Palavras-Chave | #550 Earth sciences & geology |
| Tipo |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed |
