GEOCHRONOLOGY AND FORMATION SUBDIVISIONS OF THE LOWER PRECAMBRIAN IN THE NORTHWESTERN LADOGA REGION

Citation
Vi. Shuldiner et al., GEOCHRONOLOGY AND FORMATION SUBDIVISIONS OF THE LOWER PRECAMBRIAN IN THE NORTHWESTERN LADOGA REGION, Stratigraphy and geological correlation, 4(3), 1996, pp. 220-230
Citations number
33
Categorie Soggetti
Geology,Paleontology
ISSN journal
08695938
Volume
4
Issue
3
Year of publication
1996
Pages
220 - 230
Database
ISI
SICI code
0869-5938(1996)4:3<220:GAFSOT>2.0.ZU;2-R
Abstract
A brief geological review of the northwestern Ladoga region and system atics of the Lower Precambrian subdivisions in this territory are pres ented. The respective stratigraphic scale and supplementary geologic s cheme include the following stratigraphic and metamorphic units applic able in cartography: (I)the 2700-Ma-old North Ladoga granite-gneiss as sociation of the Archean; (2) the Sortavala Group with lower metaclast ic and upper metatholeiitic subgroups of the Lower Karelian (Jatulian, Ludicovian), which are 2120-1980 Ma old; and (3) the Ladoga Group of the Upper Karelian (Kalevian) metaturbidites, which are 1910-1880 Ma o ld. Eight metamorphic suites of the Lahdenpohja Group are referred to the undivided Ludicovian-Kalevian. The Late Karelian plutonic rocks ar e subdivided into the following units: the Kurkijoki and Lauvatsaari-I mpiniemi complexes of the early orogenic stage (1880-1860 Ma) represen ted by metanorite-enderbite and metadiorite-tonalite associations resp ectively; the Tervu metadiorite-granite complex of the late orogenic s tage (1830-1810 Ma); and the Ojajarvi monzonite-granite association (1 800-1760 Ma) of postorogenic origin. Geological relations between thes e subdivisions in metamorphic zones of the Ladoga region and pertinent geochronological problems are discussed.