Abstract The Central Asian Orogenic Belt (CAOB) is the largest accretionary orogen in the
world with considerable Phanerozoic juvenile crustal growth. The eastern segment of the …

The Argun massif is an important micro-continent in the eastern Central Asian Orogenic Belt
and hosts a wide variety of Mesozoic hydrothermal Cu (–Mo), Pb–Zn–Ag, and Au deposits …

The paper presents a new understanding of the geologic composition and geodynamic
evolution of the Mongol–Okhotsk Fold Belt. It considers the issues related to recognition and …

As the core of NE China blocks (ie, Songliao, Jiamusi-Khanka, Erguna, **ng'an), the
Songliao Block plays an important role in understanding the Precambrian evolutionary …

Late Paleozoic granites of the Angara-Vitim batholith (AVB) occupy an area of 200,000 km 2
in Western Transbaikalia (the eastern part of the Central Asian fold belt). Batholith granitoids …

The geostructural, petrological, geochemical, geochronological and biostratigraphic studies
were conducted in the Hentei-Dauria fold system of the Mongolia-Okhotsk orogenic belt …

Монголо-Охотский складчатый или орогенный пояс (МОСП) выделен академиком АЕ
Ферсманом в 1926 г. протягивается на расстояние свыше 3000 км в виде непрерывной …

В результате проведенных структурно-геологических, петролого-геохимических,
геохронологических и биостратиграфических исследований установлено, что …

Based on new data on the geology, composition, U–Pb isotopic age, and paleomagnetism
of the metavolcanic rocks of the Kataevo Formation, we consider the geodynamic conditions …

Eastern Transbaikalia is a unique rare-metal province of Russia. Most of the studied
deposits are associated with granitoid intrusions. Despite the high degree of knowledge of …