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
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.