... are in agreement with published data on high-grade granites of rheomorphic domes in the neighboring region of the Yablonovy Range (Khilok-Vitim zone). The palingenic granite formation in the West-Stanovoy zone must be related to the geodynamic evolution of the latter in a setting of active continental margin...

... on amphibole and 112±3 Ma on biotite [ 4 ]. Potassium-argon ages of pegmatitic and leucocratic, often gneissic, granites within the Yablonovy granite-gneiss dome range between 110 and 140 Ma [ 7 ], or Early Cretaceous. Metamorphism and intrusion may have been synchronous. Injecting small portions of magma...

... paleogeodynamic reconstructions of the region. Carboniferous granitoids might have formed either during the development of a “transform” margin at the shifts of the Yablonovy terrane along the ACM of the Paleo-Siberian continent or under the effect of within-plate mantle plume, which gave rise to the Angara-Vitim...

... from the course of the Lena River in the west to the shores of the Bering Sea in the east, and from the Arctic Ocean in the north to the Sea of Okhotsk in the south. This is a region of varied relief, inasmuch as long and very high mountain ranges (some of the summits exceeding 3,000 meters) alternate...

... with the long-range impact of processes from the collision of the North China (Amurian–North China) block with the Siberian continent in the Mesozoic era is proposed. The Zagan MСС was formed in the Cretaceous period on the southern flank of a high mountain uplift of Western Transbaikalia, composed of late...

.... Kotelnich Anticline Siktivan—Kirov—Cheboksari Anticline Polometz-Urjum Anticline Glazov-UIianovsk Anticline Perm-Jiguli-Kuznetsk Anticline Ishimbaevo Anticline Sizran Anticline Zaborov prospect Sizran oil field—1937 Troekurov prospect Yablonovi Ovrag oil field—1937...

... (<1 km 2 ) lakes in the southern Vitim Plateau ( Fig. 1 А). The lake system is located within the Beklemishev intermontane basin at an elevation of 945–965 m asl between the Yablonovy Range in the southeast and the Osinovy Range in the northwest. The Beklemishev basin, about 130 km long and 3–15 km...

... involved in postaccretional processes. For instance, island arcs, micro continents, and active and passive margins of stabilized continents are classified as tectonic zones. Most of the Daurian zone consists of granitoids ranging in age from Ordovician-Silurian to Late Jurassic. In roof pendants, high...

... features relative to Yellowknife. The two large PA+P phases observed by Wright and Muirhead (1969) appeared to originate below the Tannu Ola and Yablonovy mountain ranges of central Asia. Using the six prominent Pa-P arrivals of Tables 5 and 6, reflection points have been determined and plotted in Figure 6...

... et al. 2001 ; Davis et al. 2001 ; Zhai et al. 2004 ). On the basis of geophysical data and petrological studies of mantle xenoliths recovered from Mesozoic to Cenozoic basalts, the current lithosphere thickness ranges from 70 to 120 km (Fan and Menzies 1992 ; Menzies et al. 1993 ; Zhang 2005...

... tourmaline in Eurasia. The pegmatites are in the southern foothills of the Malkhan Range, in the southwestern part of the Malkhan–Yablonovy (Malkhan) structural zone of Caledonian folding along the northwestern edge of a zoned magmatic area comprising the Khentey–Dauria batholith core in its center and rift...