The origin of shape preferred orientations in mylonite: inferences from in-situ experiments on polycrystalline norcamphor
| Data(s) |
1998
|
|---|---|
| Identificador |
http://boris.unibe.ch/73899/1/1-s2.0-S019181419800011X-main.pdf Herwegh, Marco; Handy, M.R. (1998). The origin of shape preferred orientations in mylonite: inferences from in-situ experiments on polycrystalline norcamphor. Journal of structural geology, 20(6), pp. 681-694. Pergamon 10.1016/S0191-8141(98)00011-X <http://dx.doi.org/10.1016/S0191-8141(98)00011-X> doi:10.7892/boris.73899 info:doi:10.1016/S0191-8141(98)00011-X urn:issn:0191-8141 |
| Idioma(s) |
eng |
| Publicador |
Pergamon |
| Relação |
http://boris.unibe.ch/73899/ |
| Direitos |
info:eu-repo/semantics/restrictedAccess |
| Fonte |
Herwegh, Marco; Handy, M.R. (1998). The origin of shape preferred orientations in mylonite: inferences from in-situ experiments on polycrystalline norcamphor. Journal of structural geology, 20(6), pp. 681-694. Pergamon 10.1016/S0191-8141(98)00011-X <http://dx.doi.org/10.1016/S0191-8141(98)00011-X> |
| Palavras-Chave | #550 Earth sciences & geology |
| Tipo |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed |
| Formato |
application/pdf |
