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Vol 194
Pages:
104-111
Download volume:
RUS
Article

Peculiiarities of geodynamic development оf the devonian graben at Spitsbergen archipelago

Authors:
A. N. Sirotkin1
D. V. Nikitin2
About authors
  • 1 — Ph.D. senior geologist Polarmarine geological exploration expedition
  • 2 — Ph.D. associate professor Saint Petersburg State Mining University
Date submitted:
2010-12-08
Date accepted:
2011-02-05
Date published:
2011-12-30

Abstract

The new data on geology of Devonian graben and subjacent complexes allow reviewing the evolution of geodynamic processes in this region during Riphean-Paleozoic. It was confirmed that Cambrian – Early Silurian series were formed in the platform environment under conditions of stable dome-like uplifting of the territory, and the subalkaline granitoids (S2-D1) may be classified as anorogenic intrusion. Devonian riftogenesis was a sequel of regeneration of the Riphean paleo- rift in conditions of general spreading. There are distinguished three stages in formation of the graben: pre-graben, orogenic and post-orogenic ones, with description of complexes formed at those stages. Concluding processes of this type are related to formation of fluorite-barite-рolymetallic occurrences and alkaline-ultrabasic dykes (D3) in zones of deep faults. The conclusion is made that the crust block, representing basement of the Barenz-sea plate in the region, has gone through the recurrent intra-plate riftogenesis in the Middle Paleozoic.

Область исследования:
(Archived) Current problems in geology and exploration of mineral deposits
Keywords:
Devonian graben Precambrian basement structural-substantial complex Paleozoic geodynamic paleo-rift deep fault stage of formation ore occurrence Spitsbergen
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References

  1. Barkhatov B.P. The main stages in tectonic development of Spitsbergen archipelago // Leningrad State University Journal. 1970. N 6. Issue 1. P.157-159.
  2. Burov Yu.P., Semevsky D.V. Principal features of tectonic structure of Devonian graben (Spitsbergen island) // Geology of Svalbard. Leningrad, 1976. P.103-117.
  3. Evdokimov A.N. Volcanoes of Spitsbergen. Saint Petersburg, 2000. 123 p.
  4. Evdokimov A.N., Sirotkin A.N., Burnaeva M.Yu., Radina E.S. The first finding of accessory minerals of kimberlites in mafite-ultramafic dykes of Spitsbergen // Rep. of the Russian Academy of Sciences. 2006. Vol.407. N 2. P.275-279.
  5. Kosteva K.N., Teben’kov A.M. Stratigraphy of Ordovician-Silurian deposits of the Saint-Jeorge fiord district (Spitsbergen archipelago) // Geology of the polar areas of the Earth: Theas. of rep. Мoscow, 2009. Vol.1. P.297-301.
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  8. Leonov Yu.G. Tectonic nature of Devonian orogenesis. Мoscow, 1976. 192 p.
  9. Lithodynamics and minerageny of sedimentary basins. Edit. by A.D.Shcheglov. Saint Petersburg, 1998. 479 p.
  10. Milanovsky E.E. Rift zones of continents. Мoscow, 1976. 279 p.
  11. Murashev L.G., Pchelina T.M., Semevsky D.V. New data on appearance of volcanism in the Low Devonian and Upper Triassic formations of the West Spitsbergen Island // Geology of Spitsbergen. Leningrad, 1983. P.96-101.
  12. Murashov L.G., Mokin Yu.I. Stratigraphic separation of Devonian sediments of Spitsbergen Island // Geology of Svalbard. Leningrad, 1976. P.78-92.
  13. Sirotkin A.N. Sedimentary-volcanogenic complex of the Middle Riphean as an indicator of the riftogenesis process in the north-west part of the Barenz sea plate basement (Spitsbergen archipelago) // Volcanism and geodynamics: Materials of the 4 th All-Russian symposium on volcanology and paleo-volcanology. Petropavlovsk-Kamchatsky, 2009. Vol.2. P.515-519.
  14. Sirotkin A.N. Evolution of regional metamorphism in complexes of the Spitsbergen crystalline basement // Geology of the Earth’s polar areas: Thes. rep. Мoscow, 2009.Vol.2. P.179-183.

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