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Vol 107

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Vol 108
Article
  • Date submitted
    1985-07-11
  • Date accepted
    1985-09-27
  • Date published
    1986-12-31

Horizon as a provincial stratigraphic subdivision

Article preview

The most important result of the study of stratigraphy of any geological region and the foundation of all geological constructions is the regional stratigraphic scheme.

How to cite: Kagarmanov A.K. Horizon as a provincial stratigraphic subdivision // Journal of Mining Institute. 1986. Vol. 107. p. 3-10.
Article
  • Date submitted
    1985-07-09
  • Date accepted
    1985-09-08
  • Date published
    1986-12-31

New representatives of Clathrodictyidae Kuhn from the Silurian of Tuva

Article preview

The Ordovician and Silurian stromatoporates of Tuva are known thanks to the studies of V. N. Ryabinin, V. I. Yavorsky, and O. V. Bogoyavlenskaya. In the process of monographic study of stromatoporites, a significant distribution of representatives of the family Clathrodictyidae was established, many of which can be of considerable help in interregional correlations.

How to cite: Bogoyavlenskaya O.V. New representatives of Clathrodictyidae Kuhn from the Silurian of Tuva // Journal of Mining Institute. 1986. Vol. 107. p. 11-16.
Article
  • Date submitted
    1985-07-11
  • Date accepted
    1985-09-18
  • Date published
    1986-12-31

Comparative characterization of the Silurian rugosas of the Siberian Platform of the Altai Mountains and Tuva

Article preview

The purpose of this paper is to review and compare rugose coral complexes in synchronous Silurian sediments of Tuva, the Altai Mountains, and the Siberian Platform.

How to cite: Sytova V.A. Comparative characterization of the Silurian rugosas of the Siberian Platform of the Altai Mountains and Tuva // Journal of Mining Institute. 1986. Vol. 107. p. 17-25.
Article
  • Date submitted
    1985-07-26
  • Date accepted
    1985-09-03
  • Date published
    1986-12-31

Issues of paleobiogeography and stratigraphy of the Silurian of Tuva in connection with new data on brachiopods of the Chergak series

Article preview

By the early 1980s, a monographic description of the main groups of organic remains from the Chergak series of Tuva had been largely completed and published: stromatoporates, tabulates, rugosas, bryozoans, crinoids.

How to cite: Vladimirskaya E.V., Eltysheva R.S., Krivobodrova A.V., Kratayte-Talimaa V.N., Chekhovich V.D. Issues of paleobiogeography and stratigraphy of the Silurian of Tuva in connection with new data on brachiopods of the Chergak series // Journal of Mining Institute. 1986. Vol. 107. p. 26-35.
Article
  • Date submitted
    1985-07-10
  • Date accepted
    1985-09-24
  • Date published
    1986-12-31

Definitive list of Devonian colonial rugosas of the USSR (code species key)

Article preview

The coding of morphological features of skeletal elements of rugosas as a basis for determinants was first applied by N. J. Spassky in 1971. Unlike the generic code key, in which qualitative differences were recorded, the proposed species key also includes quantitative parameters characterizing the morphology of the skeleton of corallites.

How to cite: Spassky N.Y. Definitive list of Devonian colonial rugosas of the USSR (code species key) // Journal of Mining Institute. 1986. Vol. 107. p. 36-40.
Article
  • Date submitted
    1985-07-29
  • Date accepted
    1985-09-21
  • Date published
    1986-12-31

Definitive list of Devonian solitary rugosa of the USSR (coded species key)

Article preview

The coding of morphological characters of the rugose skeleton as a basis for the subsequent determination of the taxon from suborder to genus inclusive was first proposed in the article by N.Ya, Spassky in 1971. Subsequent experience of application showed the high efficiency of this methodology, significantly reducing the time of training, specialists and the very definition of species.

How to cite: Kravtsov A.G. Definitive list of Devonian solitary rugosa of the USSR (coded species key) // Journal of Mining Institute. 1986. Vol. 107. p. 41-45.
Article
  • Date submitted
    1985-07-26
  • Date accepted
    1985-09-30
  • Date published
    1986-12-31

Rugoses from the Kamenka Bay horizon of the southern part of Novaya Zemlya

Article preview

The Kamenka Bay horizon is the lowest regional stratigraphic unit of the Devonian on Novaya Zemlya. Within the southern part of the archipelago (Vaigach-Yuzhno-Novaya Zemlya structural-facial zone) it includes a thick (700-1000 m) stratum of terrigenous-carbonate formations, which is divided into three formations (from bottom to top): the Propaschinskian, West Nogorskian and Karandean.

How to cite: Lakhov G.V. Rugoses from the Kamenka Bay horizon of the southern part of Novaya Zemlya // Journal of Mining Institute. 1986. Vol. 107. p. 46-51.
Article
  • Date submitted
    1985-07-10
  • Date accepted
    1985-09-27
  • Date published
    1986-12-31

New Devonian spiriferids of Transcaucasia

Article preview

Spiriferidae occupy a prominent place in the brachiopod complexes of Devonian sediments of Transcaucasia. Biostratigraphic studies undertaken by the author in the 1980s, allowed to clarify their composition and establish new species and subspecies.

How to cite: Grechishnikova I.A. New Devonian spiriferids of Transcaucasia // Journal of Mining Institute. 1986. Vol. 107. p. 52-60.
Article
  • Date submitted
    1985-07-04
  • Date accepted
    1985-09-13
  • Date published
    1986-12-31

Some Devonian trilobites of Transcaucasia

Article preview

It is known that the Devonian of Transcaucasia, represented by the Upper Ems and all stages of the middle and upper sections, is characterized by a variety of trilobites. The latter form a complex of at least 35 forms, most of which are new species.

How to cite: Levitsky E.S. Some Devonian trilobites of Transcaucasia // Journal of Mining Institute. 1986. Vol. 107. p. 61-66.
Article
  • Date submitted
    1985-07-20
  • Date accepted
    1985-09-15
  • Date published
    1986-12-31

Emian pachydomellids (ostracods) of the western Zeravshan Range

Article preview

Representatives of the family Pachydomellidae were widely distributed in shallow areas of Paleozoic marine basins. Central Asian species were found in the Kitab horizon on the left bank of the Jindydarya River.

How to cite: Mikhailova E.D. Emian pachydomellids (ostracods) of the western Zeravshan Range // Journal of Mining Institute. 1986. Vol. 107. p. 67-75.
Article
  • Date submitted
    1985-07-27
  • Date accepted
    1985-09-05
  • Date published
    1986-12-31

Zhivetes sea lilies of the eastern slope of the Southern Urals

Article preview

The studied crinoidea were recovered from tuffaceous sandstones of the lower part of the Zhyvegian Stage, zone Stringocephalus burtini, from a Middle Devonian section on the right bank of the Musogatka River (Ural River basin), 15 km north of Novoorsk.

How to cite: Polyarnaya Z.A. Zhivetes sea lilies of the eastern slope of the Southern Urals // Journal of Mining Institute. 1986. Vol. 107. p. 76-81.
Article
  • Date submitted
    1985-07-14
  • Date accepted
    1985-09-11
  • Date published
    1986-12-31

Characterization of the Artinskian Stage of the Orenburg Urals by foraminifers

Article preview

The team of the stratigraphopaleontological party of the Leningrad Mining Institute under the direction of V. P. Pnev since 1973 has been engaged in a detailed study of the sections of deep oil exploration wells drilled by the Orenburg Production and Geological Association in the Orenburg Priuralsky area.

How to cite: Polozova A.N. Characterization of the Artinskian Stage of the Orenburg Urals by foraminifers // Journal of Mining Institute. 1986. Vol. 107. p. 82-87.
Article
  • Date submitted
    1985-07-19
  • Date accepted
    1985-09-10
  • Date published
    1986-12-31

Discontinuity of formation of the Paleozoic complex in the south of the Pre-Ural marginal trough

Article preview

In the Orenburg Urals, within the central and western, instrumental with the Russian platform part of the Pre-Ural marginal trough, there are carried out prospecting and exploration works for oil and gas, productive horizons of which are confined mainly to sediments of Permian and Carboniferous age.

How to cite: Pnev V.P. Discontinuity of formation of the Paleozoic complex in the south of the Pre-Ural marginal trough // Journal of Mining Institute. 1986. Vol. 107. p. 88-91.
Article
  • Date submitted
    1985-07-22
  • Date accepted
    1985-09-17
  • Date published
    1986-12-31

The genus Arctohungarites (Ammonoidea) from the Middle Triassic of the Boreal Region

Article preview

Representatives of the genus Arctohungarites are widely distributed in the Anisian sediments of the Boreal paleobiogeographic region. Most of the known species originate from the northeastern regions of the USSR and only one from North America.

How to cite: Arkadyev V.V. The genus Arctohungarites (Ammonoidea) from the Middle Triassic of the Boreal Region // Journal of Mining Institute. 1986. Vol. 107. p. 92-97.
Article
  • Date submitted
    1985-07-25
  • Date accepted
    1985-09-23
  • Date published
    1986-12-31

Triassic marine lilies of the Koryak Plateau

Article preview

Three stages are outlined in the development of sea lilies of the Mediterranean and Pacific provinces of the USSR. The first, corresponding to the Indus Age and Early Olenecian time of the Early Triassic, is the period of origin of the Mesozoic, crinoid fauna.

How to cite: Klikushin V.G. Triassic marine lilies of the Koryak Plateau // Journal of Mining Institute. 1986. Vol. 107. p. 98-101.