...M.E. Kazimirovsky Detailed petrochemical characteristics of Paleozoic (Cambrian(?)-Silurian and Carboniferous) granitoids of the West Stanovoy structure-formational zone (SFZ) (central Selenga-Stanovoy mountain area (SSMA), Transbaikalia) are presented. The Early Paleozoic granitoids...

... , V.P. , Sal’nikova , E.B. , Yarmolyuk , V.V. , Velikoslavinskii , S.D. , Yakovleva , S.Z. , Plotkina , Yu.V. , 2015 . Granitoids of the Olekma Complex in the Selenga–Stanovoi super-terrane of the central Asian mobile belt: Age and tectonic position . Dokl. Earth Sci. 464 ( 1...

... fold belt; 7 , Cenozoic loose sediments; 8 , major faults. Letters indicate tectonic blocks (terranes) in superterranes of the Central Asian Fold Belt. Selenga–Stanovoi superterrane: AG, Amazar–Gilyui; MG, Mogocha; TN, Tungir. Dzhugdzur–Stanovoi superterrane: BR, Bryanta; DM, Dambuki; IL, Ilikan; KP...

... of the Siberian Platform ( Fig. 1 ). The CAFB and the investigated part of the framing of the Siberian Platform to the west and south include the Caledonian Selenga–Stanovoi, Late Paleozoic–Early Cretaceous Mongol-Okhotsk orogenic belts and the Argun–Mamyn microcontinent (Karsakov and Zhao Chunjing, 2001...

... of the granitoids of the Amudzhikan complex (134–132 Ma) located within the Selenga–Stanovoy superterrane is the same as the age of the granitoids of the Upper Amur and Burinda complexes (140– 127 Ma) widespread within the Argun terrane ( Sorokin et al., 2004 , 2009 , 2010a ). The wide occurrence of the Late...

... . Early Cretaceous collisional granitoids of the Drevnestanovoi complex from the Selenga–Stanovoi superterrane of the Central Asian Mobile Belt . Dokl. Earth Sci. 456 ( 2 ), 649 – 654 . Kravchinsky , V.A. , Sorokin , A.A. , 2001 . Paleomagnetism of Devonian rocks in the Ol’doi terrane...

..., upon the granitoids of the Tynda–Bakaran complex, and upon the Precambrian metamorphic rocks of the Zverevo block of the Stanovoi structural suture. This suture separates the Aldan Shield of the Siberian craton from the Dzhugdzhur–Stanovoi and Selenga–Stanovoi superterranes in the Central Asian...

... massifs; 2 — Dzhugdzhur-Stanovoy superterrane; 3 , 4 — Selenga-Stanovoy (West Stanovoy) superterrane: 3 — Mogocha block, 4 — Urkan block; 5 — Dzheltulak suture zone; 6 — Kerulen-Argun-Mamyn terrane; 7 — Mongolo-Okhotsk fold belt; 8 — faults: a — major, b — subsidiary; massifs: 1...

.../S0016852113050026 . Kotov , A.B. , Larin , A.M. , Sal’nikova , E.B. , Velikoslavinskii , S.D. , Glebovitskii , V.A. , Sorokin , A.A. , Yakovleva , S.Z. , Anisimova , I.V. , 2014 . Early Cretaceous collisional granitoids of the Drevnestanovoi complex from the Selenga-Stanovoi...

... the Yablonovyi–Malkhan and West Stanovoi zones of metamorphic and cratonic terranes. The latter, in turn, border the Mongolia–Okhotsk suture in the southeast and the associated large shear zones that separate the terranes from the Argun cratonic terrane and from the belt of Middle–Late Paleozoic turbidite...

...I.V. Buchko; A.A. Sorokin; V.A. Ponomarchuk; A.E. Izokh Abstract The Lukinda dunite–troctolite–gabbro massif in the Selenga–Stanovoy superterrane on the southeastern framing of the Siberian Platform was earlier considered Precambrian. The performed 40 Ar/ 39 Ar dating of the massif plagioclase...

... ). The Aga–Shilka terrane has sedimentary (Late Paleozoic–Mesozoic) and sedimentary-metamorphic (Riphean–Paleozoic) layers up to 3–4 km (sometimes, 5–6 km) in thickness. The Selenga–Stanovoi superterrane is formed predominantly by Upper Archean–Lower Proterozoic granite-gneisses (upper 4–5 km thick layer...

... production from concentrations of radioactive elements measured in situ for the upper crust; for the middle crust, we used mean U and Th abundances in high-grade Precambrian rocks exposed within the Aldan–Stanovoi and Sinian–Korean shields and in Precambrian terranes (microcontinents) of the Central Asian...

.... [ 2 ], 8 — after Belichenko et al. [ 3 ], 9 — after Khomentovsky [ 4 ]. Terranes: Dz — Dzhida, Er — Eravna, Ik — Ikat, Br — Barguzin, Ol — Ol’khon, Kh — Khamar-Daban, TM — Tuvino-Mongolian, BM — Baikal-Muya, Ok — Olokit, WS — West Stanovoi. SC — Siberian craton, MO — Mongolian-Okhotsk belt...

... anomalies ( Fig. 1 , b). Thus, the Western Stanovoy (Geological map…, 1986) (or the Selenga-Stanovoy ( Krasny et al., 1999 )) geoblock in northeastern Transbaikalia does not belong to the Stanovoy terrane. It is more reasonable to relate it to the Baikal-Vitim terrane ( Gusev and Khain, 1995 ), which...

... Cretaceous coal-bearing continental sediments. It overlies the Paleozoic and older basement rocks with a sharp angular unconformity. The Strelka and Malaya Tynda sedimentary basins, which are shallower, are located inside the Selenga–Stanovoi orogenic belt, at its boundary with the Mongol–Okhotsk belt...