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Vol 5 Iss. 1
Pages:
57-67
Download volume:
RUS
Article

Dunits of Vasilyevo - Shaitanskaya dacha in the Urals

Authors:
D. Misharev
Date submitted:
1913-07-16
Date accepted:
1913-09-21
Date published:
1914-01-01

Abstract

Shaitanskaya Dacha is located on the very ridge of the southern part of the Middle Urals, included in Sheet 138 of the general geological map of Russia. To the south, the dacha is bordered by the Chusovaya River, which serves as a natural boundary with Revdinskaya Dacha; to the north and west, it adjoins Bilimbaevskaya Dacha, and to the east, Verkh-Isetskaya Dacha. The western chain consists of individual mountains: Volchikha and the three Magnitnye mountains. The former is composed of gabbro, while the others are composed of amphibolites. The eastern chain, known under the name Grebni (The Ridges), is a purely serpentine range, in the very center of which there are outcrops of primary igneous rocks of ultrabasic magma: dunites and pyroxenites, interconnected by transitional rocks. Let us assign the dunites to the olivine subgroup (see the article).

Область исследования:
(Archived) Articles
Funding:

None

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References

  1. Zaitsev. Trudy Geologicheskogo Komiteta, Vol. IV. (in Russian)
  2. N. Smirnov. Zapiski Uralskogo Ob-va lubitelei estestvoznaniya, Vol. XXX. (in Russian)
  3. V. V. Nikitin. Geological Investigations of the Central Group of Dachas of the Verkh-Isetsk Factories, the Revdinskaya Dacha, and the Murzinsky Area. (Trudy Geologicheskogo Komiteta, New Series, Issue 22). (in Russian)
  4. L. Duparc et F. Pearce. Recherches géologiques et petrographiques sur l'Oural du Nord.
  5. Levinson-Lessing. Geological Sketch of the South-Zaozerskaya Dacha and Denezhkin Kamen in the Northern Urals. (in Russian)
  6. Rosenbusch–Wülfing. Mikroskopische Physiographie. II, 1st Half, p. 475.
  7. L. Duparc et F. Pearce. Recherches géologiques et petrographiques sur l'Oural du Nord. I, p. 163.
  8. L. Duparc. Platinum and Platinum Deposits in the Urals. Mining Journal, 1913, Vol. I.
  9. Levinson-Lessing. p. 166.
  10. V. Nikitin. Geological Investigations of the Central Group of Dachas of the Verkh-Isetsk Factories, the Revdinskaya Dacha, and the Murzinsky Area. Tr. Geol. Kom., New Ser., Issue 22, p. 109. (in Russian)
  11. Doelter. Handbuch der Mineralchemie, pp. 295–302.
  12. L. Duparc et F. Pearce. Recherches géologiques et petrographiques sur l'Oural du Nord, Vol. I, p. 159.
  13. A. Boldyrev. Diagrams Relating the Birefringence Values of Principal Sections and the Value of the Optic Axial Angle. Zap. Imp. Min. Ob., XLVIII, Issue 1. (in Russian)
  14. Rosenbusch – Wülfing. Mikroskopische Physiographie. II. 1. Half, p. 475.
  15. L. Duparc et Th. Hornung. Sur une nouvelle théorie de l'ouralitisation. (Comptes rendus, Juill. 1904).
  16. L. Duparc. Sur la transformation du pyroxen en amphibole (Bull. Soc. Franç. de Mineral. 1908).
  17. Levinson-Lessing. On a New Platinum Deposit in the Urals (in the Siniye Gory). Izv. SPb. Pol. Inst., 1909, Issue 2, pp. 433–437. (in Russian)
  18. E. Fedorov and V. Nikitin. Bogoslovsky Mining District, p. 142. (in Russian)
  19. V. Nikitin. Geological Investigations of the Central Group of Dachas of the Verkh-Isetsk Factories, the Revdinskaya Dacha, and the Murzinsky Area, pp. 80 and 113. (in Russian)
  20. L. Duparc. Platinum and Platinum Deposits in the Urals. M. J., 1913, Vol. I, p. 41. (in Russian)
  21. V. Nikitin. Geological Investigations of the Central Group of Dachas of the Verkh-Isetsk Factories, the Revdinskaya Dacha, and the Murzinsky Area, pp. 39–42. (in Russian)

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