Выдержка
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 A relict dynamometamorphosed quartz is described in the primary rocks, which have been replaced by apatite-carbonate ores.-D.A.B.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 оригинала | Русский |
|---|---|
| Название основной публикации | Mineralogicheskii Zhurnal |
| Страницы | 57-63 |
| Число страниц | 7 |
| Том | 5 |
| Издание | 1 |
| Состояние | Опубликовано - 1983 |
Отпечаток
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Цитировать
(The orientation and peculiarities of formation of apatite crystals in the Seligdar deposit.). / Boyarko, G. Y.
Mineralogicheskii Zhurnal. Том 5 1. ред. 1983. стр. 57-63.Результат исследований: Материалы для книги/типы отчетов › Глава
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TY - CHAP
T1 - (The orientation and peculiarities of formation of apatite crystals in the Seligdar deposit.)
AU - Boyarko, G. Y.
PY - 1983
Y1 - 1983
N2 - 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 A relict dynamometamorphosed quartz is described in the primary rocks, which have been replaced by apatite-carbonate ores.-D.A.B.
AB - 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 A relict dynamometamorphosed quartz is described in the primary rocks, which have been replaced by apatite-carbonate ores.-D.A.B.
UR - http://www.scopus.com/inward/record.url?scp=0021067525&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0021067525&partnerID=8YFLogxK
M3 - Глава
AN - SCOPUS:0021067525
VL - 5
SP - 57
EP - 63
BT - Mineralogicheskii Zhurnal
ER -