CRYSTALLIZATION OF THE KYMI TOPAZ GRANITE STOCK WITHIN THE WIBORG RAPAKIVI GRANITE BATHOLITH, FINLAND: EVIDENCE FROM MELT INCLUSIONS

2009 ◽  
Vol 47 (6) ◽  
pp. 1359-1374 ◽  
Author(s):  
S. Lukkari ◽  
R. Thomas ◽  
I. Haapala
2020 ◽  
Vol 486 (1) ◽  
pp. 67-76 ◽  
Author(s):  
Andrey Bulakh ◽  
Paavo Härmä ◽  
Elena Panova ◽  
Olavi Selonen

AbstractRapakivi granites were in use during the Middle Ages in Finland. Their most spectacular use, however, was for structures built in St Petersburg between 1760 and 1917. Remarkable examples are the majestic and slender Alexander Column and the 112 columns of St Isaac's Cathedral. All Rapakivi granite was extracted from the Wiborg Rapakivi granite batholith in several quarries around the municipality of Virolahti in SE Finland (old Russia). Today, the 1640 Ma-old Wiborg batholith is the most important area for natural stone production in Finland and in the Leningrad region, Russian Federation. The main quarried stone varieties of Rapakivi granite (Baltic Brown, Baltic Green, Carmen Red, Karelia Red, Eagle Red and Balmoral Red) are regularly produced in large quantities in Finland for the global stone market due to the stone's unique qualities. Examples of applications in Rapakivi granite from Finland can be found in the USA, China, South Africa, the UK, Italy, Austria, Ireland, Spain and Germany as well as in Scandinavia and Russia. There are also quarries near Vyborg, the Russian Federation: Vozrozhdenie and Ala-Noskua.


2005 ◽  
Vol 142 (1) ◽  
pp. 23-30 ◽  
Author(s):  
MINGGUO ZHAI ◽  
ZHIYAO NI ◽  
CHANG WHAN OH ◽  
JINGHUI GUO ◽  
SEON GYU CHOI

A large rapakivi granite batholith in the Neo-Archaean/Palaeoproterozoic Odesan complex, northeastern Gyeonggi massif, South Korea, has been dated at 1839±10 Ma using SHRIMP U–Pb analysis of zircons. The age, petrological and geochemical characteristics of this batholith are similar to those of the rapakivi granite batholiths exposed in the Rangnim massif of North Korea and in the Miyun–Chengde complex of North China. The country rocks of these rapakivi granite batholiths are also comparable; all are composed of granitic gneisses and banded iron formation (BIF)-bearing supracrustal rocks metamorphosed to amphibolite- to granulite-facies. This study provides new evidence for the suggestion that the Gyeonggi and Rangnim massifs may share an affinity with the Precambrian basement of the North China craton. The study provides new insight into the possible eastward extension of the Sulu orogenic belt in the Korean peninsula and further provides evidence to correlate the Korea basement to a possible global 2.1–1.8 Ga supercontinent.


2009 ◽  
Vol 96 (1) ◽  
pp. 53-68 ◽  
Author(s):  
Fredrik Karell ◽  
Carl Ehlers ◽  
Meri-Liisa Airo ◽  
Olavi Selonen

2008 ◽  
Vol 95 (0) ◽  
pp. 78-80
Author(s):  
Fredrik Kareil ◽  
Carl Ehlers ◽  
Olavi Selonen ◽  
Meri-Liisa Airo

2017 ◽  
Vol 58 (12) ◽  
pp. 2493-2517 ◽  
Author(s):  
Aku P Heinonen ◽  
O Tapani Rämö ◽  
Irmeli Mänttäri ◽  
Tom Andersen ◽  
Kirsi Larjamo

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