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Vol 28
Pages:
117-128
Download volume:
RUS
Article
Geology

Types of quartz veins of the Urals and their rock crystal potential

Authors:
A. E. Karyakin
Date submitted:
1952-07-25
Date accepted:
1952-09-12
Date published:
1953-01-01

Abstract

Three systems of jointing cracks predominate in the rocks of the crystal-bearing strip of the Northern Urals: concordant, intersecting and transverse. Almost all crystal-bearing quartz veins of the Northern Urals are confined to these cracks. Among the quartz veins of the Northern Urals, the first two types are most common. Transverse quartz veins are less common. It should be noted that the division of quartz veins into the listed types is conditional, since they are all of the same age, genetically related and fill a system of three interconnected tectonic cracks

Область исследования:
Geology
Keywords:
veins crystal-bearing bands
Funding:

None

Go to volume 28

References

  1. Grigoriev D. P., How are mineral druses formed, Priroda, 1947, No. 9. (in Russian)
  2. Karyakin A. E., Genetic connection of crystal nests with quartz veins and the origin of cavities, Zapiski Gornogo instituta , 1949, p. XXIII. (in Russian)
  3. Karyakin A. E., On the connection between the quality of quartz crystals and their external appearance, Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva , 1948, No. 4. (in Russian)
  4. Merkulova G. V., On the type and abundance of piezoelectric quartz deposits in the Subpolar Urals, Izvestiya AN SSSR , geological series, 1942, No. 3. (in Russian)

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