dc.contributor.author | Banks, Nigel L. | |
dc.coverage.spatial | 20341 Hal'kavarri | |
dc.date.accessioned | 2020-08-26T13:10:18Z | |
dc.date.available | 2020-08-26T13:10:18Z | |
dc.date.issued | 1973 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674953 | |
dc.description.abstract | The increasing abundance of trace fossils in the ?late Precambrian to Lower Cambrian sediments of the Dividal Group is comparable with that found in the laterally equivalent but much thicker succession to the east and provides further evidence of the gradual but rapid development of metazoan life at that time. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (288) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | FOSSIL | |
dc.subject | STRATIGRAFI | |
dc.subject | GEOKRONOLOGI | |
dc.subject | PALEONTOLOGI | |
dc.subject | PETROGRAFI | |
dc.subject | SEDIMENTÆR BERGART | |
dc.title | Trace fossils in the Halkkavarre section of the Dividal Group (?late Precambrian - Lower Cambrian), Finnmark. | |
dc.type | Journal article | |
dc.description.localcode | 35257 | |
dc.source.pagenumber | 1-6 | |