(The orientation and peculiarities of formation of apatite crystals in the Seligdar deposit.)

Translated title of the contribution: Russian with English abstract

Research output: Chapter in Book/Report/Conference proceedingChapter

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Abstract

Descriptions are given of minerals in the Seligdar deposit, central Aldan region, which have crystallized in an anisotropic stress field. These minerals form linear and linear-planar aggregates, and braided and banded structures in the rocks. The clearly defined stressed nature of the apatite is demonstrated, showing in the formation of stunted pseudo-orthorhombic, pseudo-monoclinic, pseudo-triclinic and spiral forms of crystals. A relict dynamometamorphosed quartz is described in the primary rocks, which have been replaced by apatite-carbonate ores.-D.A.B.

Original languageRussian
Title of host publicationMineralogicheskii Zhurnal
Pages57-63
Number of pages7
Volume5
Edition1
Publication statusPublished - 1983

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ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

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