Ferruginous quartzite formation in the crystalline basement of the Nepa-Botuoba anteclise, Republic of Sakha (Yakutia)
https://doi.org/10.52349/0869-7892_2022_89_22-32
Abstract
Mineralogical and petrographic characteristics of hematite-magnetite ore discovered by two oil prospecting wells in the dome of the Nepa-Botuoba anteclise at a depth of about 1,5 km are discussed for the first time. Geological conditions of two deep-seated iron deposits are identified; they suggest that the latter probably belong to the Archean-Proterozoic ferruginous quartzite formation. The important role of this formation in the Early Vendian geomorphogenesis is shown. Results of U-Pb dating of zircons from granitoids surrounding ferruginous quartzite obtained from three wells are presented. The derived ages corresponding to the crystallization of melts parental for granitoids (2005 ± 12, 1969 ± 13, and 1857 ± 6 Ma) indicate their Early Proterozoic age. On the basis of the obtained materials, probable relationship of the described formation with the Late Archean-Early Proterozoic Borsalinsky Series, widespread in the Aldan Shield, was suggested.
About the Authors
V. G. Kolokol’tsevRussian Federation
Kolokol’tsev Vyacheslav Grigor’evich – Candidate of Geological and Mineralogical Sciences, Leading Researcher
74 Sredny Prospect, St. Petersburg, 199106
I. V. Osadchiy
Russian Federation
Osadchiy Il’ya Vladimirovich – Head of Department
74 Sredny Prospect, St. Petersburg, 199106
A. N. Khabarov
Russian Federation
Khabarov Andrey Nikolaevich – Head of Department
74 Sredny Prospect, St. Petersburg, 199106
References
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Review
For citations:
Kolokol’tsev V.G., Osadchiy I.V., Khabarov A.N. Ferruginous quartzite formation in the crystalline basement of the Nepa-Botuoba anteclise, Republic of Sakha (Yakutia). Regional Geology and Metallogeny. 2022;1(89):22-32. (In Russ.) https://doi.org/10.52349/0869-7892_2022_89_22-32