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Vol 200
Pages:
342-346
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RUS
Article

Injective sand bodies in lower permian deposits of Novaya Zemlya

Authors:
R. A. Shchekoldin
About authors
  • Ph.D. associate professor National Mineral Resources University (Mining University)
Date submitted:
2012-07-10
Date accepted:
2012-09-06
Date published:
2013-04-16

Abstract

Geological setting, composition and morphology of injective sandy bodies in Lower Permian deposits of the south part of Novaya Zemlya are described. Formation of these bodies is interpreted as a result of liquefaction of sandy beds and extrusion of the formed suspension into the host clayey sediments. This process was caused by high sedimentation rates in a prograding submarine fan environment fed with siliciclastics from the rising Urals orogene to the south of Novaya Zemlya.

Область исследования:
(Archived) Geology and metallogeny
Keywords:
Novaya Zemlya Lower Permian sand dykes
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References

  1. Sobolev N.N., Schekoldin R.A. Unified regional scheme of the Upper Devonian deposits of Novaya Zemlya // Geology of the South island of Novaya Zemlya / PGO «Sevmorgeologiya». Leningrad, 1982. Р.5- 24.
  2. Pickering K.T., Stow D.A.V., Watson M.P. and Hiscott R.N. Deep-water facies, processes and models: a review and classification scheme for modern and ancient sediments // Earth Sci. Rev. 1986. 23. Р.75- 174.
  3. Lowe D.R. Sediment gravity flows: Their classification and some problems of application to natural flows and deposits // Soc. econ. Paleont. Miner. Spec. Publ. 1979. 25. Р.75- 82.
  4. Lowe D.R. Sediment gravity flows: II. Depositional models with special reference to the deposits of high-density turbidity currents // J.Sediment. Petrol. 1982. 52. Р.279- 298.
  5. Schekoldin R.A., Sobolev N.N. and Matveev V.P. Carboniferous deposits of the southern area of Novaya Zemlya // Newsletter on Carboniferous Stratigraphy. 1994. 12. Р.17- 20.
  6. Schekoldin R.A. Upper Devonian-Carboniferous deep -water deposits of Novaya Zemlya // Proceedings of the Ist Latin American congress of Sedimentology. 1997. V.2. Р.265- 270.

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