NEW DATA ON THE GEOLOGICAL STRUCTURE OF THE SYNNYR ULTRA-K INTRUSIVE FORMATION

The Synnyrsky massif is the largest intrusive containing ultra-potassium syenites, synnyrites, which are raw materials for the production of potash fertilizers and aluminum. An extensive complex of geological and geochemical studies has been carried out, including exploratory drilling, which was carried out on the massif for the first time. The data obtained made it possible to significantly change the idea of the structure of the massif, including a different look at the regularities of the placement of potash-alumina ores, significantly increasing the ore potential and the reliability of its assessment. The present study discusses the existence within the Synnyrsky complex of the third, previously undetected, large intrusive phase, which has its own geological and geochemical features

НОВЫЕ ДАННЫЕ О ГЕОЛОГИЧЕСКОМ СТРОЕНИИ СЫННЫРСКОГО УЛЬТРАКАЛИЕВОГО ИНТРУЗИВНОГО МАССИВА

The Synnyrsky massif is the largest intrusive containing ultra-potassium syenites, synnyrites, which are raw materials for the production of potash fertilizers and aluminum. An extensive complex of geological and geochemical studies has been carried out, including exploratory drilling, which was carried out on the massif for the first time. The data obtained made it possible to significantly change the idea of the structure of the massif, including a different look at the regularities of the placement of potash-alumina ores, significantly increasing the ore potential and the reliability of its assessment. The present study discusses the existence within the Synnyrsky complex of the third, previously undetected, large intrusive phase, which has its own geological and geochemical features.Сыннырский массив – крупнейший интрузив, содержащий в своем составе ультракалиевые сиениты, сынныриты, являющиеся сырьем для производства калийных удобрений и алюминия. Выполнен обширный комплекс геолого-геохимических исследований, в том числе поисково-разведочное бурение, которое было проведено на массиве впервые. Полученные данные позволили существенным образом изменить представление о строении массива, в том числе иначе взглянуть на закономерности размещения калийно-глиноземных руд, значительно увеличив рудный потенциал и достоверность его оценки. В настоящем исследовании обсуждается существование в пределах Сыннырского комплекса третьей, ранее не выделяемой, крупной интрузивной фазы, которая имеет свои геолого-геохимические особенности

U-Pb detrital zircon geochronology and provenance of Neoproterozoic sedimentary rocks in southern Siberia: New insights into breakup of Rodinia and opening of Paleo-Asian Ocean

© 2018 International Association for Gondwana Research We present the synthesis of new data on detrital zircon geochronology of the Neoproterozoic strata of the southern part of the Siberian craton as well as a comprehensive analysis of previously published stratigraphic, sedimentological and geochronological (LA-ICP-MS) data obtained for key sections in this area that allows us to trace the process of birth and early stages of development of the Paleo-Asian Ocean (PAO). Before the break-up of Rodinia and opening of PAO, Tonian – Cryogenian intracontinental sedimentary basin existed between southern Siberia and northern Laurentia. The detachment of the southern flank of the Siberian craton from northern Laurentia and opening of the PAO between these cratons took place in Cryogenian. The detrital zircon ages from lower parts of Neoproterozoic successions suggest the Siberian craton as the sole provenance area right after the opening of the PAO. The age constraints on the lower parts of the studied Neoproterozoic successions, which are based on correlation of their tillite horizons with the Marinoan glaciation, suggest the late Cryogenian age for these sedimentary rocks. A clear change in the age spectra of detrital zircons from “unimodal” (Early Precambrian only) in older sedimentary rocks to “bimodal” (Early Precambrian as well as Neoproterozoic) in younger sequences of the studied successions marks the next stage of the PAO evolution. The abundance of youngest (630–610 Ma) detrital zircons in the upper parts of the studied sequences reflects a shrinkage of the oceanic basin as a result of the convergence of the craton with the microcontinents and island arcs within the Paleo-Asian Ocean. We suggest that a passive oceanic margin along the southern margin of the Siberian craton has been transformed into a series of foreland basins at ~610 Ma