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In Sikhote Alin, the Anuy river provides a representative cross-section of the pre-Eocene structure of the area east of the central Sikhote Alin fault. The Mesozoic rocks are divided into the following groups, from bottom to top: Anuy metamorphic rocks; the Tithonian-Berriasian (Samarkinsk) accretionary complex; Early Cretaceous (Zhuravlevsk-Tumnin) turbidite; and mid-Cretaceous Al-rich (Khungariisk)...