Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #96406:
- #96406
Main publication details
MARC recordMetamorphism of ultramafic rocks in the Central Scandinavian Caledonides / Kurt Bucher-Nurminen.
| Title: | Metamorphism of ultramafic rocks in the Central Scandinavian Caledonides / Kurt Bucher-Nurminen. |
| Author(s): | Bucher-Nurminen, Kurt. |
| Date: | 1988. |
| In: | Norges Geologiske Undersøkelse. Special Publication. (1988.), Vol. 3 (1988) |
| Abstract: | Lenses and boudins represent parts of dismembered ophiolite sequences and bits of sub-continental upper mantle. Metaperidotites are isofacial with metamorphic envelope, usually metasediments but also metagranitoids. Metamorphic assemblages co-define regional metamorphic gradient of prograde metamorphism. Maximum temperature was too low to replace calcic amphibole by calcic pyroxene. Regional distribution of assemblages in ultramafic rocks defines regular pattern crossing nappe boundaries. |
| Notes: | Norges Geologiske Undersøkelse. Special Publication. Vol. 3 :86-95 (1988). |
| Keywords: | 551.1/.4 -- Geology. 552.4 -- Metamorphic rocks. B -- Geology and soil sciences. (*3) -- Arctic regions. (*58) -- Norway. |
| SPRI record no.: | 96406 |
LDR 01322naa#a2200000#a#4500 001 SPRI-96406 005 20230322222553.0 007 ta 008 230322s1988####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-96406 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBucher-Nurminen, Kurt. 245 10 ‡aMetamorphism of ultramafic rocks in the Central Scandinavian Caledonides /‡cKurt Bucher-Nurminen. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1988. 300 ## ‡ap. 86-95 :‡bdiags., maps. 500 ## ‡aNorges Geologiske Undersøkelse. Special Publication. Vol. 3 :86-95 (1988). 520 3# ‡aLenses and boudins represent parts of dismembered ophiolite sequences and bits of sub-continental upper mantle. Metaperidotites are isofacial with metamorphic envelope, usually metasediments but also metagranitoids. Metamorphic assemblages co-define regional metamorphic gradient of prograde metamorphism. Maximum temperature was too low to replace calcic amphibole by calcic pyroxene. Regional distribution of assemblages in ultramafic rocks defines regular pattern crossing nappe boundaries. 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a552.4 -- Metamorphic rocks.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*58) -- Norway.‡2udc 773 0# ‡7nnas ‡tNorges Geologiske Undersøkelse. Special Publication. ‡gVol. 3 (1988) ‡wSPRI-84344 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230322