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Record #110663:

Early Proterozoic layered intrusions and related ore deposits in the northern part of the Fennoscandian Shield / Tuomo T. Alapieti, Jarmo J. Lahtinen.

Title: Early Proterozoic layered intrusions and related ore deposits in the northern part of the Fennoscandian Shield / Tuomo T. Alapieti, Jarmo J. Lahtinen.
Author(s): Alapieti, Tuomo T.
Lahtinen, Jarmo J.
Date: 1991.
In: Geologiska Föreningens i Stockholm Förhandlingar. (1991.), Vol. 113(1) (1991)
Abstract: Only one intrusion (Kukkola) has been encountered in Sweden so far; number of intrusions and intrusion fragments exceeds 20 in Finland, concentrated principally in two areas: in discontinuous belt at latitude of northern end of Gulf of Bothnia and in central Finnish Lapland. In USSR they occur on Kola Peninsula (Kol'skiy Poluostrov), in Paanajärvi area and on north-eastern side of Lake Onega (Onezhskoye Ozero). Examples of all characteristic ore types have been found. Two types of parental magma have tentatively been proposed.
Notes:

Geologiska Föreningens i Stockholm Förhandlingar. Vol. 113(1) :40-42 (1991).

Keywords: 551.7 -- Stratigraphy.
551.72 -- Proterozoic.
553 -- Economic geology.
553.042 -- Mineral resources.
B -- Geology and soil sciences.
(*50) -- Soviet Union.
(*531.9) -- Murmanskaya Oblast'.
(*56) -- Finland.
(*561) -- Finnish Lapland.
(*57) -- Sweden.
(*571.1) -- Norrbottens lan.
SPRI record no.: 110663

MARCXML

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001 SPRI-110663
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007 ta
008 240415s1991####xx####|##|###|0||#0|eng#d
035 ## ‡aSPRI-110663
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aAlapieti, Tuomo T.
245 10 ‡aEarly Proterozoic layered intrusions and related ore deposits in the northern part of the Fennoscandian Shield /‡cTuomo T. Alapieti, Jarmo J. Lahtinen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 40-42.
500 ## ‡aGeologiska Föreningens i Stockholm Förhandlingar. Vol. 113(1) :40-42 (1991).
520 3# ‡aOnly one intrusion (Kukkola) has been encountered in Sweden so far; number of intrusions and intrusion fragments exceeds 20 in Finland, concentrated principally in two areas: in discontinuous belt at latitude of northern end of Gulf of Bothnia and in central Finnish Lapland. In USSR they occur on Kola Peninsula (Kol'skiy Poluostrov), in Paanajärvi area and on north-eastern side of Lake Onega (Onezhskoye Ozero). Examples of all characteristic ore types have been found. Two types of parental magma have tentatively been proposed.
650 07 ‡a551.7 -- Stratigraphy.‡2udc
650 07 ‡a551.72 -- Proterozoic.‡2udc
650 07 ‡a553 -- Economic geology.‡2udc
650 07 ‡a553.042 -- Mineral resources.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*50) -- Soviet Union.‡2udc
651 #7 ‡a(*531.9) -- Murmanskaya Oblast'.‡2udc
651 #7 ‡a(*56) -- Finland.‡2udc
651 #7 ‡a(*561) -- Finnish Lapland.‡2udc
651 #7 ‡a(*57) -- Sweden.‡2udc
651 #7 ‡a(*571.1) -- Norrbottens lan.‡2udc
700 1# ‡aLahtinen, Jarmo J.
773 0# ‡7nnas ‡tGeologiska Föreningens i Stockholm Förhandlingar. ‡gVol. 113(1) (1991) ‡wSPRI-15270
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240415