Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?


Autoria(s): Schmaedicke, E.; Will, T.; Mezger, Klaus
Data(s)

2015

Formato

application/pdf

Identificador

http://boris.unibe.ch/81398/1/Garnet.pdf

Schmaedicke, E.; Will, T.; Mezger, Klaus (2015). Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? Lithos, 238, pp. 185-206. Elsevier 10.1016/j.lithos.2015.09.016 <http://dx.doi.org/10.1016/j.lithos.2015.09.016>

doi:10.7892/boris.81398

info:doi:10.1016/j.lithos.2015.09.016

urn:issn:0024-4937

Idioma(s)

eng

Publicador

Elsevier

Relação

http://boris.unibe.ch/81398/

Direitos

info:eu-repo/semantics/restrictedAccess

Fonte

Schmaedicke, E.; Will, T.; Mezger, Klaus (2015). Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? Lithos, 238, pp. 185-206. Elsevier 10.1016/j.lithos.2015.09.016 <http://dx.doi.org/10.1016/j.lithos.2015.09.016>

Palavras-Chave #550 Earth sciences & geology
Tipo

info:eu-repo/semantics/article

info:eu-repo/semantics/publishedVersion

PeerReviewed