skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View 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 It is no longer being updated, so does not reliably reflect our current library holdings.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:

Metamorphism 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

MARCXML

LDR 01322naa#a2200000#a#4500
001 SPRI-96406
005 20220930021908.0
007 ta
008 220930s1988####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# ‡a20220930