Publication: Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?
cris.virtual.author-orcid | 0000-0002-2443-8539 | |
cris.virtualsource.author-orcid | 2f5de103-cfa3-401d-b1a3-98833ad51afb | |
dc.contributor.author | Schmaedicke, E. | |
dc.contributor.author | Will, T. | |
dc.contributor.author | Mezger, Klaus | |
dc.date.accessioned | 2024-10-24T17:14:51Z | |
dc.date.available | 2024-10-24T17:14:51Z | |
dc.date.issued | 2015 | |
dc.description.numberOfPages | 22 | |
dc.description.sponsorship | Institut für Geologie | |
dc.identifier.doi | 10.7892/boris.81398 | |
dc.identifier.publisherDOI | 10.1016/j.lithos.2015.09.016 | |
dc.identifier.uri | https://boris-portal.unibe.ch/handle/20.500.12422/141524 | |
dc.language.iso | en | |
dc.publisher | Elsevier | |
dc.relation.ispartof | Lithos | |
dc.relation.issn | 0024-4937 | |
dc.relation.organization | DCD5A442C18FE17DE0405C82790C4DE2 | |
dc.subject.ddc | 500 - Science::550 - Earth sciences & geology | |
dc.title | Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? | |
dc.type | article | |
dspace.entity.type | Publication | |
dspace.file.type | text | |
oaire.citation.endPage | 206 | |
oaire.citation.startPage | 185 | |
oaire.citation.volume | 238 | |
oairecerif.author.affiliation | Institut für Geologie | |
unibe.contributor.role | creator | |
unibe.contributor.role | creator | |
unibe.contributor.role | creator | |
unibe.description.ispublished | pub | |
unibe.eprints.legacyId | 81398 | |
unibe.journal.abbrevTitle | LITHOS | |
unibe.refereed | TRUE | |
unibe.subtype.article | journal |
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