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Record #135683:
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MARC recordGranites from the base of the Lapland Granulite Belt as a geochemical analogue to the Rapakivi-type granites / Evgeni Terekhov, Valery Levitski.
| Title: | Granites from the base of the Lapland Granulite Belt as a geochemical analogue to the Rapakivi-type granites / Evgeni Terekhov, Valery Levitski. |
| Author(s): | Terekhov, Evgeni. Levitski, Valery. |
| Date: | 1995. |
| Publisher: | Trondheim, Norway: Geological Survey of Norway |
| In: | Geology of the Eastern Finnmark - Western Kola Peninsula Region. (1995.), |
| Abstract: | Pink medium- to coarse-grained microline granites and migmatites occur widely at base of belt. Protolith is Archaean, but in Early Proterozoic they were uplifted from deep crustal levels and thrust onto lower-grade rocks of different age and composition. Granites are mainly foliated, forming sill- like bodies of chemical composition similar to Rapakivi granites. A-type nature suggests that they originated from partial melting by hot, deep-rooted fluids during thrusting. |
| 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. 550.4 -- Geochemistry. 551.1/.4 -- Geology. 552.321.1 -- Granite. B -- Geology and soil sciences. (*3) -- Arctic regions. (*531.9) -- Murmanskaya Oblast'. (*582) -- Finnmark. |
| SPRI record no.: | 135683 |
LDR 01705naa#a2200000#a#4500 001 SPRI-135683 005 20230923045158.0 007 ta 008 230923s1995####no#ab##|#####|1||#0#eng#d 035 ## ‡aSPRI-135683 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTerekhov, Evgeni. 245 10 ‡aGranites from the base of the Lapland Granulite Belt as a geochemical analogue to the Rapakivi-type granites /‡cEvgeni Terekhov, Valery Levitski. 260 ## ‡aTrondheim, Norway :‡bGeological Survey of Norway,‡c1995. 300 ## ‡ap. 185-192 :‡bdiags., tables, map. 500 ## ‡aIn: Geology of the Eastern Finnmark - Western Kola Peninsula Region / David Roberts, Øystein Nordgulen, eds. 520 3# ‡aPink medium- to coarse-grained microline granites and migmatites occur widely at base of belt. Protolith is Archaean, but in Early Proterozoic they were uplifted from deep crustal levels and thrust onto lower-grade rocks of different age and composition. Granites are mainly foliated, forming sill- like bodies of chemical composition similar to Rapakivi granites. A-type nature suggests that they originated from partial melting by hot, deep-rooted fluids during thrusting. 650 07 ‡a061.3 -- Conferences: 1993 1st. International Barents Symposium.‡2udc 650 07 ‡a550.4 -- Geochemistry.‡2udc 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a552.321.1 -- Granite.‡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# ‡aLevitski, Valery. 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# ‡a20230923