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Vol 158
Pages:
186-190
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Genetic basis for the development of criteria of diamondiferous kimberlite bodies

Authors:
A. V. Kozlov1
Yu. S. Korobeinikova2
About authors
  • 1 — G.V. Plekhanov Saint Petersburg Mining Institute
  • 2 — G.V. Plekhanov Saint Petersburg Mining Institute
Date submitted:
2003-08-17
Date accepted:
2003-09-26
Date published:
2004-03-01

Abstract

The model of formation of pipe-like kimberlite and lamproite bodies, which is based on the fluid dynamic regime of development of magmatic paleosystems, is developed. The main factors determining the fluid dynamic regime of formation of kimberlite bodies are formulated. The proposed model satisfactorily explains many morphological features of kimberlite systems represented by dykes, pipes and sills, peculiarities of the internal structure of kimberlite bodies composing them and may serve as the basis for developing criteria of their diamond potential.

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References

  1. Джейкс А. Кимберлиты и лампроиты Западной Австралии / А.Джейкс, Дж.Луис, К.Смит. М.: Мир, 1989.
  2. Каминский Ф.В. Новый генетический тип промышленно-алмазоносных пород – лампроиты Западной Австралии // Экономика минерального сырья и геолого-разведочных работ / ВИЭМС. М., 1987.
  3. Козлов А.В. Роль природной флотации при образовании магматических месторождений алмазов / А.В.Козлов, В.Н.Зинченко // Материалы конференции «Алмазы-50» / ВСЕГЕИ. СПб, 2004.
  4. Милашев В.А. Трубки взрыва. Л.: Недра, 1984.
  5. Милашев В.А. Кимберлиты и глубинная геология. Л.: Недра, 1990.
  6. Попов В.Е. Генезис вулканогенно-осадочных месторождений и их прогнозная оценка. Л.: Недра, 1991.
  7. Минеральные ресурсы мира на начало 1999 г. / МПР РФ, ФГУНПП «Аэрогеология». М., 2000.

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