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Tampere schist belt

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Journal Article
Published: 01 September 2014
Journal of the Geological Society (2014) 171 (5): 659-671.
... dipping reverse faults are less common (e.g. Nguyen et al . 1998 ; Piessens et al . 2002 ). The Tampere Schist Belt in southern Finland is a c . 1.92–1.88 Ga volcano-sedimentary basin that underwent inversion and closure at c . 1.89–1.88 Ga ( Fig. 1 ; Patchett & Kouvo 1986 ; Kähkönen et...
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Overall structure of the eastern part of the central <b>Tampere</b> <b>Schist</b> <b>Belt</b> (s...
Published: 01 September 2014
Fig. 2. Overall structure of the eastern part of the central Tampere Schist Belt (see Fig. 1 for location and for key; in addition, S, Sorila; Pi, Pirttiniemi). U–Pb zircon age data are indicated (in billions of years; see text for references). Figure compiled and modified from Nironen (1989
Journal Article
Journal: Economic Geology
Published: 01 November 2003
Economic Geology (2003) 98 (7): 1329-1353.
..., attributed to the formation and accretion of a number of volcanic arcs adjacent to the Karelian craton, is associated with syngenetic massive sulfide mineralization, commonly with gold grades between 0.1 and 1.0 ppm. The Tampere schist belt in southern Finland, which formed within this accretionary setting...
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Journal Article
Journal: Economic Geology
Published: 01 December 1996
Economic Geology (1996) 91 (8): 1335-1353.
...M. Poutiainen; P. Groenholm Abstract The Kutemajrvi gold telluride deposit is located about 200 km north of Helsinki in southwestern Finland. It occurs in the continental island arc-type Paleoproterozoic volcano-sedimentary Tampere schist belt situated in the central part of the Svecofennian domain...
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F ig . 8. Surface geology and two cross sections at Kutemajärvi, <b>Tampere</b> s...
Published: 01 November 2003
F ig . 8. Surface geology and two cross sections at Kutemajärvi, Tampere schist belt. After Poutiainen and Grönholm (1996) .
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( a ) Simplified geological map of the Fennoscandian shield. The <b>Tampere</b> Sc...
Published: 01 September 2014
Fig. 1. ( a ) Simplified geological map of the Fennoscandian shield. The Tampere Schist Belt (indicated with a rectangle) is located in a palaeobasin between the Early Svecofennian orogenic basement to the north and the contemporaneous supracrustal rocks to the south. 1, Phanerozoic sedimentary
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Conceptual tectonic model for the (southern) <b>Tampere</b> basin prior to and dur...
Published: 01 September 2014
slope). ( b ) Subduction and associated volcanism initiates, and leads to basin inversion and a creation of an (intra-arc) basin at c . 1.89 Ga. The volcanic activity leads to the deposition of the volcanic unit (note that the entire volcanic package in the Tampere Schist Belt is much thicker than
... which may manifest a time of convergent plate movements and closing of the oceans and rift basins. A number of Paleoproterozoic volcanic provinces, such as the Vihanti-Pyhäsalmi area and the Tampere schist belt in Finland and the Bergslagen area and Skellefte district in Sweden, are bordering...
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Journal Article
Journal: Economic Geology
Published: 01 November 2003
Economic Geology (2003) 98 (7): 1355-1369.
... Ga) Kuhmo-Suomussalmi and Ilomantsi greenstone belts and in the Paleoproterozoic (2.0–1.75 Ga) Tampere greenstone belt ( Nurmi, 1991 ; Luukkonen, 1994 ; Eilu, 1999 ). The gold deposits in these greenstone belts are analogous to mesothermal (orogenic) gold deposits in other shield areas in terms...
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Journal Article
Journal: Economic Geology
Published: 01 November 2003
Economic Geology (2003) 98 (7): 1271-1290.
..., southwest Sweden), Kutemajärvi (Tampere schist belt, southern Finland), and Pampalo (Hattu schist belt, Ilomantsi area, eastern Finland). This increased prospecting and production activity has also led to a significant increase in our knowledge of the gold-forming processes in the Fennoscandian Shield...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP321.11
EISBN: 9781862395695
... zone; OB, Outokumpu Belt; SAC, Southern Finland Arc Complex, SB, Savo Belt; TB, Tampere Belt. The box denotes the area shown in Figure 3 . Magenta lines denote the location of detailed crustal sections of Figure 7 . The NW–SE-trending Savo Arc (SA; Figs  1 a & 2 ) consists of metavolcanic...
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Map showing place names referred to in the text. Springs are represented by...
Published: 01 February 2005
Fig. 1 Map showing place names referred to in the text. Springs are represented by triangles. Ki=Kiiminki, Kn=Kirkkonummi, Ta= Tampere, Va=Vantaa, Vp=Vainospää in Utsjoki, CFGC=Central Finland Granite Complex, LLGB=Lapland Granulite Belt, PPSB=Peräpohja Schist Belt.
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F ig . 5. Photomicrographs of mineralization-related auriferous quartz vein...
Published: 01 November 2003
in tourmalinized mica schist from the Hosko prospect Ilomantsi greenstone belt). C. Coarse-grained quartz-pyrite-arsenopyrite-gold vein in sericitized host rock from the Järvenpää prospect (Tampere greenstone belt). D. Quartz-arsenopyrite-gold quartz vein with an folded apophysis in metagraywacke from
Journal Article
Published: 01 May 2001
Geochemistry: Exploration, Environment, Analysis (2001) 1 (2): 109-117.
..., Rantasalmi, southeastern Finland . Finland Geological Survey Special Paper , 25 . KÄHKÖNEN , Y. 1989 . Geochemistry and petrology of the metavolcanic rocks of the Early Proterozoic Tampere schist belt, southern Finland . Finland Geological Survey Bulletin , 345 . LIIMATAINEN , J...
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Journal Article
Published: 18 January 2010
Geological Magazine (2010) 147 (4): 551-569.
... Finland granitoid complex; TB – Tampere schist belt; PB – Pirkanmaa belt; HB – Häme schist belt; UB – Uusimaa belt; L – Loimaa area; PG – Pöytyä granodiorite; OG – Oripää granite; numbered sheared zones: 1– Kankaanpää shear zone; 2 – Pori/Kynsikangas shear zone: P – continuation of the Pori shear zone; K...
Journal Article
Published: 01 February 2009
Geochemistry: Exploration, Environment, Analysis (2009) 9 (1): 81-92.
... 480 Ojakangas R.W. An Early Proterozoic metagraywacke-slate turbidite sequence: the Tampere schist belt, southwestern Finland Bulletin of the Geological Society of Finland 1986 58 241 261 Pasieczna A. Atlas of Urban Soils Contamination in Poland 2003 Warszawa Panstwowy...
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Journal Article
Published: 01 August 2015
European Journal of Mineralogy (2015) 27 (5): 639-649.
...-bearing volcanogenic massive sulphide deposits (Pyhäsalmi and Vihanti ore districts) are associated with island-arc structures (1.91–1.87 Ga) exposed within the Raahe-Ladoga suture zone. Some features of sulphide ores in the Tampere schist belt (Kutemajärvi deposit) indicate a submarine hydrothermal...
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Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.33
EISBN: 9781862394070
.... Palaeoproterozoic Svecofennian: SaR, Satakunta Rapakivi Area; HaB, Häme Belt; PiB, Pirkkala Belt; TaB, Tampere (Schist) Belt; CFGC, Central Finland Granitoid Complex; SaB, Savo Belt; PoB, Pohjanmaa Belt; Karelian (Palaeoproterozoic rocks): KaB, Kainuu (Schist) Belt. Karelian (Archaean rocks): IC, Iisalmi Complex...
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Journal Article
Published: 01 February 2005
Geochemistry: Exploration, Environment, Analysis (2005) 5 (1): 41-50.
...Fig. 1 Map showing place names referred to in the text. Springs are represented by triangles. Ki=Kiiminki, Kn=Kirkkonummi, Ta= Tampere, Va=Vantaa, Vp=Vainospää in Utsjoki, CFGC=Central Finland Granite Complex, LLGB=Lapland Granulite Belt, PPSB=Peräpohja Schist Belt. ...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2012
GSA Bulletin (2012) 124 (3-4): 517-531.
... can be treated as weighted mean averages of detritus derived from a broad source area ( DePaolo, 1981 ; Taylor and McLennan, 1985 ; crustal residence age in terminology of O'Nions et al., 1983 ). A pre-Svecofennian crustal component is thus proxied here by 1.89 Ga Tampere schist, for which the ca...
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