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Record #135646:

Correlation of the Archaean rocks between the Sørvaranger area, Norway, and the Kola Peninsula, Russia (Baltic Shield) / Larissa F. Dobrzhinetskaya, Øystein Nordgulen, Valery R. Vetrin, John Cobbing, Brian A. Sturt.

Title: Correlation of the Archaean rocks between the Sørvaranger area, Norway, and the Kola Peninsula, Russia (Baltic Shield) / Larissa F. Dobrzhinetskaya, Øystein Nordgulen, Valery R. Vetrin, John Cobbing, Brian A. Sturt.
Author(s): Dobrzhinetskaya, Larissa F.
Nordgulen, Øystein.
Vetrin, Valery R.
Cobbing, John.
Sturt, Brian A.
Date: 1995.
Publisher: Trondheim, Norway: Geological Survey of Norway
In: Geology of the Eastern Finnmark - Western Kola Peninsula Region. (1995.),
Abstract: Rocks occur as NW-SE trending blocks of medium- to high-grade gneisses separated by shear zones and medium- to low-grade greenstone belt successions of Early Proterozoic age. Several units across border were correlated. Archaean crustal rocks were formed and reshaped during period 2.9-2.5 Ga. and from different tectonic terranes, whose boundaries are probably along major shear zones and greenstone belts.
Notes:

In: Geology of the Eastern Finnmark - Western Kola Peninsula Region / David Roberts, Øystein Nordgulen, eds.

Keywords: 061.3 -- Conferences: 1993 1st. International Barents Symposium.
550.93 -- Geochronology.
551.1/.4 -- Geology.
551.71 -- Archaean.
551.72 -- Proterozoic.
552.42 -- Gneiss.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*531.9) -- Murmanskaya Oblast'.
(*582) -- Finnmark.
SPRI record no.: 135646

MARCXML

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035 ## ‡aSPRI-135646
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245 00 ‡aCorrelation of the Archaean rocks between the Sørvaranger area, Norway, and the Kola Peninsula, Russia (Baltic Shield) /‡cLarissa F. Dobrzhinetskaya, Øystein Nordgulen, Valery R. Vetrin, John Cobbing, Brian A. Sturt.
260 ## ‡aTrondheim, Norway :‡bGeological Survey of Norway,‡c1995.
300 ## ‡ap. 7-27 :‡bdiags., tables, maps.
500 ## ‡aIn: Geology of the Eastern Finnmark - Western Kola Peninsula Region / David Roberts, Øystein Nordgulen, eds.
520 3# ‡aRocks occur as NW-SE trending blocks of medium- to high-grade gneisses separated by shear zones and medium- to low-grade greenstone belt successions of Early Proterozoic age. Several units across border were correlated. Archaean crustal rocks were formed and reshaped during period 2.9-2.5 Ga. and from different tectonic terranes, whose boundaries are probably along major shear zones and greenstone belts.
650 07 ‡a061.3 -- Conferences: 1993 1st. International Barents Symposium.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.71 -- Archaean.‡2udc
650 07 ‡a551.72 -- Proterozoic.‡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(*531.9) -- Murmanskaya Oblast'.‡2udc
651 #7 ‡a(*582) -- Finnmark.‡2udc
700 1# ‡aDobrzhinetskaya, Larissa F.
700 1# ‡aNordgulen, Øystein.
700 1# ‡aVetrin, Valery R.
700 1# ‡aCobbing, John.
700 1# ‡aSturt, Brian A.
773 0# ‡7nnam ‡aDavid Roberts, Øystein Nordgulen, eds. ‡tGeology of the Eastern Finnmark - Western Kola Peninsula Region. ‡dTrondheim, Norway : Geological Survey of Norway, 1995. ‡wSPRI-134536
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329