PALEOPROTEROZOIC GRANITOIDS OF THE CENTRAL PART OF THE NEPA-BOTUOBIYA ANTECLISE AS INDICATORS OF THE FORMATION OF THE TRANS-SIBERIAN OROGENIC BELT OF THE SIBERIAN CRATON
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DOI: 10.2113/rgg20254908
Abstract: The paper presents studies of gneisses and granitoids from three deep boreholes located in the central part of the Nepa-Botuobiya anteclise of the Siberian craton. Based on U-Pb (LA-ICP-MS) geochronological studies of zircon, the age… read more here.
Keywords: botuobiya anteclise; nepa botuobiya; central part; siberian craton ... See more keywords