Abstract The Central Asian Orogenic Belt (CAOB, also known as the Altaid Tectonic
Collage), one of the largest and long-lived accretionary orogens in the world, developed …

To better understand the subsurface behavior of subducting slabs and their relation to the
tectonic evolution of the overriding plate, we conduct a full waveform inversion on a large …

In this review we focus on the volcanism, that occurred in Transbaikalia, Siberia after the
closure of the Mongolia-Okhotsk Ocean. The closure happened in the Early Jurassic. After …

We present a 3‐D radially anisotropic model of the crust and mantle beneath East Asia
down to 900 km depth. Adjoint tomography based on a spectral element method is applied …

Detrital zircons from the Ob, Yenisey, Lena, Amur, Volga, Dnieper, Don and Pechora rivers
have been analyzed for U–Th–Pb, O and Lu–Hf isotopes to constrain the growth rate of the …

Abstract The origin of Hangai Dome, an unusual large‐scale, high‐elevation low‐relief
landform in central Mongolia, remains enigmatic partly due to lack of constraints on its …

Mantle plumes can be recognized by their magmatic expression as large igneous provinces
(LIPs). However, identification of plumes in old, structurally complicated fold belts is …

The world-class gold-ore districts of South-East Russia and North-East China are located
above the frontal and peripheral regions of subducted oceanic lithosphere accumulated as …

Abstract The South Khangai volcanic region (SKVR) comprises fields of Late Mesozoic–
Cenozoic volcanic rocks scattered over southern and central Mongolia. Evolution of the …

The contemporary horizontal movements and deformations in the central and southern parts
of the Baikal depression are analyzed, and their relationship with contemporary seismicity is …