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

Результат исследований: Материалы для книги/типы отчетовГлава

2 Цитирования (Scopus)

Аннотация

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 A relict dynamometamorphosed quartz is described in the primary rocks, which have been replaced by apatite-carbonate ores.-D.A.B.

Язык оригиналаРусский
Название основной публикацииMineralogicheskii Zhurnal
Страницы57-63
Число страниц7
Том5
Издание1
СостояниеОпубликовано - 1983

    Fingerprint

ASJC Scopus subject areas

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

Цитировать

Boyarko, G. Y. (1983). (The orientation and peculiarities of formation of apatite crystals in the Seligdar deposit.). В Mineralogicheskii Zhurnal (1 ред., Том 5, стр. 57-63)