Rotated garnets: a mechanism to explain the high frequency of inclusion trail curvature angles around 90° and 180°


Autoria(s): Trouw, Rudolph A.J.; Tavares, Felipe M.; Robyr, Martin
Data(s)

2008

Formato

application/pdf

Identificador

http://boris.unibe.ch/84586/1/1-s2.0-S0191814108000874-main.pdf

Trouw, Rudolph A.J.; Tavares, Felipe M.; Robyr, Martin (2008). Rotated garnets: a mechanism to explain the high frequency of inclusion trail curvature angles around 90° and 180°. Journal of structural geology, 30(8), pp. 1024-1033. Pergamon 10.1016/j.jsg.2008.04.011 <http://dx.doi.org/10.1016/j.jsg.2008.04.011>

doi:10.7892/boris.84586

info:doi:10.1016/j.jsg.2008.04.011

urn:issn:0191-8141

Idioma(s)

eng

Publicador

Pergamon

Relação

http://boris.unibe.ch/84586/

Direitos

info:eu-repo/semantics/restrictedAccess

Fonte

Trouw, Rudolph A.J.; Tavares, Felipe M.; Robyr, Martin (2008). Rotated garnets: a mechanism to explain the high frequency of inclusion trail curvature angles around 90° and 180°. Journal of structural geology, 30(8), pp. 1024-1033. Pergamon 10.1016/j.jsg.2008.04.011 <http://dx.doi.org/10.1016/j.jsg.2008.04.011>

Palavras-Chave #550 Earth sciences & geology
Tipo

info:eu-repo/semantics/article

info:eu-repo/semantics/publishedVersion

PeerReviewed