Fluid-explosion ultramafic rocks of the Middle Timan dyke complex and their paragenetic association with carbonatite
Abstract
Fluid-explosion structure, including carbonatite, explosive ultramafic rocks of the dyke complex and alkaline metasomatite, has been identified in the Middle Timan. Fluid-explosion structure was formed due to carbonatite magmatism and its fluid derivatives.
About the Authors
I. I. Golubeva
Institute of geology Komi UB RAS
Russian Federation
Russian Federation
Candidate of Geological and Mineralogical Sciences, Senior Researcher
D. N. Remizov
A. P. Karpinsky Russian Geological Research Institute (VSEGEI)
Russian Federation
Russian Federation
Doctor of Geological and Mineralogical Sciences, Deputy Head of the Sector
I. N. Burtsev
Institute of geology Komi UB RAS
Russian Federation
Russian Federation
Candidate of Geological and Mineralogical Sciences, Interim Director
V. N. Filippov
Institute of geology Komi UB RAS
Russian Federation
Russian Federation
Senior Researcher
A. S. Shuyskiy
Institute of geology Komi UB RAS
Russian Federation
Russian Federation
Junior Researcher
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Review
For citations:
Golubeva I.I., Remizov D.N., Burtsev I.N., Filippov V.N., Shuyskiy A.S. Fluid-explosion ultramafic rocks of the Middle Timan dyke complex and their paragenetic association with carbonatite. Regional Geology and Metallogeny. 2019;(80):30–44. (In Russ.)
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