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Vol 12 No 2
Pages:
33-52
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RUS
Research article
Articles

Phenomena of assimilation and hybridism in alkaline rocks of Tagoba-Sobak

Authors:
I. K. Nikitin
Date submitted:
1938-08-22
Date accepted:
1938-10-16
Date published:
1939-02-01

Abstract

From field observations and the study of the stone material at our disposal, it follows that in the magmatic process of formation of alkaline rocks of Tagoba-Sobak, three phases are established, replacing each other in the usual sequence: 1) the intrusive phase, represented by syenites, 2) vein - aplite and albitite, 3) phase of intensive manifestation of the process of pneumatolysis, completing magmatic activity. The last phase is associated with the formation of sodalite, cancrinite and other pegmatites and the automorphic change of rocks of early phases, expressed in intensive metasomatic replacement of primary minerals and leading to the formation of sodalite- and cancrinite- nepheline syenites. The change in the chemical composition of magma from early to late phases was expressed: 1) in the depletion of ferruginous-magnesian components: 2) in the enrichment of the magmatic melt with sodium and silicic acid and 3) in the concentration of mineralizers - F, CL, etc. By comparing the mineralogical composition of various xenoliths, on the one hand, and the mineralogical composition of xenoliths with that of typical biotite-nepheline syenites, on the other, one can be convinced that between the extreme member of the xenolith (vesuvian hybrid) and the biotite-nepheline syenite there is a connection and there are gradual transitions of one rock type to another (see article).

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References

  1. Записки Спб. Мин. Общ., т. XIX, 193, 1883.
  2. Записки Спб. Мин. Общ,, сер, 2, ч. 31, 1894.
  3. Мушкетов И.В. -- Геологическая экспедиция на Зеравшанский ледник в 1880 г., т. II, Туркестан, 1906.
  4. Марковский А.П. -- Основные черты геологического строения средней части центрального Таджикистана. Тр. ТКЭ. 1934.
  5. Никитин И.К. -- Петрографический очерк маршрутной съемки на северном склоне Туркестанского хребта, Гос. Н.-техн. Геол. Разв. Изд., 1933.
  6. Никитин И.К. -- К геологии северного склона Туркестанского хребта. Таджикско-Памирская экспедиция 1934 г., вып. L. Труды экспедиции.
  7. Никитин И.К. -- Геологическое строение верховьев Зеравшана и Западного Каратегина. (Фонды ЦНИГРИ, рукопись.)
  8. Преображенский И.А.-- Нефелиновые сиениты верховьев р. Тагобы-Собак в бассейне верхнего Зеравшана. Изв. СПБ. Политехнич. инст., т. XV, 1911.
  9. Соболевский В.Н. -- Нефелиновые сиениты верховьев Зеравшана. Сборник
  10. Таджикская Комплексная Экспедиция 1932 г. Госхимтехиздат, 1933.

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