Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Hege Fonneland"'
Publikováno v:
Sedimentary Geology. 238:254-267
Detrital zircon U–Pb and Lu–Hf isotope data from Neoproterozoic to Cretaceous sandstones exposed in eastern Greenland, 70°30′–74°N, are reported to characterize and evaluate the provenance from Greenland during pre-breakup and post-breakup
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c244ef6649506c29f3b721fffdc0dea
https://doi.org/10.1016/j.sedgeo.2011.04.018
https://doi.org/10.1016/j.sedgeo.2011.04.018
Publikováno v:
The Island Arc. 14:517-541
The Solund-Stavfjord ophiolite complex (SSOC) in western Norway represents a remnant of the Late Ordovician oceanic lithosphere, which developed in an intermediate- to fast-spreading Caledonian back-arc basin. The internal architecture and magmatic f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f22a7b7aea1ea742a578783130896ad7
https://doi.org/10.1111/j.1440-1738.2005.00481.x
https://doi.org/10.1111/j.1440-1738.2005.00481.x
Publikováno v:
Sedimentary Geology. 164:147-159
The provenance of Cretaceous to Paleocene sandstones from the Norwegian Sea has been determined by laser ablation ICPMS U–Pb and Pb–Pb dating of detrital zircons. The zircon grains were extracted from sandstones sampled in the More and the Voring
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7822d5c1ad7be98966c8fd5df6dfdaf7
https://doi.org/10.1016/j.sedgeo.2003.09.005
https://doi.org/10.1016/j.sedgeo.2003.09.005
Publikováno v:
Chemical Geology. 182:605-618
New developments in U–Pb dating of zircons by laser ablation (LA) ICPMS are described and, for the first time, a direct comparison of detrital zircons dated by LA ICPMS and SIMS methods is presented. True real-time mass bias correction is made by a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::956bb06d4cfc70005ae9515cfa605bcb
https://doi.org/10.1016/s0009-2541(01)00341-2
https://doi.org/10.1016/s0009-2541(01)00341-2
Publikováno v:
Contributions to Mineralogy and Petrology
Xenotime overgrowths on detrital zircon in siliciclastic sediments have been reported in numerous studies. However, in natural samples, solid solution of zircon and xenotime is limited to near-end-member compositions. In order to characterize the int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3ca41fc21f50b3e86dbbaf5a9cca42ac
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:246111
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:246111
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.