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Record #150761:
- #150761
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MARC recordThe late Palaeozoic Eskolabreen granitoids of southern Ny Friesland, Svalbard Caledonides - geochemistry, age and origin / Åke Johansson, David G. Gee.
| Title: | The late Palaeozoic Eskolabreen granitoids of southern Ny Friesland, Svalbard Caledonides - geochemistry, age and origin / Åke Johansson, David G. Gee. |
| Author(s): | Johansson, Åke. Gee, David G. |
| Date: | 1999. |
| In: | GFF. (1999.), Vol. 121(2) (1999) |
| Abstract: | Eskolabreen Complex of Finlandveggen Nappe is lowermost exposed tectonostratigraphic unit in these Caledonides. It is banded sequence, mostly of interlayered granitic gneisses and concordant amphibolites. U-Pb zircon dating was suppplemented by new readings. Sm-Nd analyses yield εNd values near -1. Data suggest that all granitoid units represent same suite of late Palaeoproterozoic within-plate granites, intruded into and largely derived from pre-existing continental crust. |
| Notes: | GFF. Vol. 121(2) :113-126 (1999). |
| Keywords: | 54.027 -- Isotope analysis. 550.4 -- Geochemistry. 551.1/.4 -- Geology. 551.72 -- Proterozoic. 551.73 -- Palaeozoic. 552.42 -- Gneiss. B -- Geology and soil sciences. (*3) -- Arctic regions. (*32) -- Svalbard. |
| SPRI record no.: | 150761 |
LDR 01457naa#a2200000#a#4500 001 SPRI-150761 005 20240418054656.0 007 ta 008 240418s1999####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-150761 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aJohansson, Åke. 245 14 ‡aThe late Palaeozoic Eskolabreen granitoids of southern Ny Friesland, Svalbard Caledonides - geochemistry, age and origin /‡cÅke Johansson, David G. Gee. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1999. 300 ## ‡ap. 113-126 :‡bill., diags., tables, maps. 500 ## ‡aGFF. Vol. 121(2) :113-126 (1999). 520 3# ‡aEskolabreen Complex of Finlandveggen Nappe is lowermost exposed tectonostratigraphic unit in these Caledonides. It is banded sequence, mostly of interlayered granitic gneisses and concordant amphibolites. U-Pb zircon dating was suppplemented by new readings. Sm-Nd analyses yield εNd values near -1. Data suggest that all granitoid units represent same suite of late Palaeoproterozoic within-plate granites, intruded into and largely derived from pre-existing continental crust. 650 07 ‡a54.027 -- Isotope analysis.‡2udc 650 07 ‡a550.4 -- Geochemistry.‡2udc 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.72 -- Proterozoic.‡2udc 650 07 ‡a551.73 -- Palaeozoic.‡2udc 650 07 ‡a552.42 -- Gneiss.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*32) -- Svalbard.‡2udc 700 1# ‡aGee, David G. 773 0# ‡7nnas ‡tGFF. ‡gVol. 121(2) (1999) ‡wSPRI-128316 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418