Diamond potential of the lower carboniferous deposits on the western part of the Siberian platform

Author:

AKULOV N. I.1ORCID,GLADKOV A. S.1ORCID,GROMOVA I. A.1ORCID

Affiliation:

1. Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences

Abstract

In this study, we aimed to investigate the fundamental problem of identifying the role of lithological and paleogeographic settings on ancient platforms during the development of diamond-forming systems at the turn of the Middle Paleozoic (D3–C1) tectonic and magmatic reconstruction. The main focus was on the stratigraphy of the Carboniferous (Mississippian) deposits, the paleogeographic conditions of their accumulation, and their diamond-bearing reservoirs. The lithological and paleogeographic maps provided in this article show the locations of the sedimentary basins and other landscape zones, which allow the identification of demolition areas of terrigenous materials and delineate attractive areas for diamond prospecting activity.

Publisher

Academy of Sciences of the Republic of Sakha (Yakutia)

Subject

General Medicine

Reference51 articles.

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2. Akulov N.I. Facial analysis of the Upper Paleozoic intermediate reservoirs of the Angarida diamonds. Sovetskaya geologiya [Soviet Geology]. 1990. 1990;(5):48–56 (In Russ.)

3. Akulov N.I. Buried Upper Paleozoic diamond-bearing placers of Angarida. Geology of intermediate diamond reservoirs. Vladimirov B.M. et al (ed.). Irkutsk; 1991: 41–44. (In Russ.)

4. Akulov N.I. Paleogeographic prerequisites for the search for the Middle Paleozoic primary sources of diamonds in the south of the Siberian Platform. Izvestiya Vuzov Sibiri. 1999;4-5:116–118. (In Russ.)]

5. Akulov N.I., Misharina V.A., Mashchuk I.M. Early Carboniferous age and lake genesis of the Tushama horizon (Siberian platform). Russian Geology and Geophysics. 2000;41(10):1443–1453. (In Russ.)

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