Standard

(Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield). / Bulakh, A. G.; Zolotarev, A. A.; Bobrova, I. P.; Gulii, V. N.; Vande- Kirkov, Y. V.

In: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, Vol. 113, No. 4, 1984, p. 398-410.

Research output: Contribution to journal › Article › peer-review

Harvard

Bulakh, AG, Zolotarev, AA, Bobrova, IP, Gulii, VN & Vande- Kirkov, YV 1984, '(Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield).', Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, vol. 113, no. 4, pp. 398-410.

APA

Bulakh, A. G., Zolotarev, A. A., Bobrova, I. P., Gulii, V. N., & Vande- Kirkov, Y. V. (1984). (Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, 113(4), 398-410.

Vancouver

Bulakh AG, Zolotarev AA, Bobrova IP, Gulii VN, Vande- Kirkov YV. (Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1984;113(4):398-410.

Author

Bulakh, A. G. ; Zolotarev, A. A. ; Bobrova, I. P. ; Gulii, V. N. ; Vande- Kirkov, Y. V. / (Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield). In: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1984 ; Vol. 113, No. 4. pp. 398-410.

BibTeX

@article{50e2ec34e044444d93342acfd3cf4d0c,
title = "(Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield).",
abstract = "Apatite-bearing rocks in this deposit in Precambrian gneisses and schists contain on average 18% apatite, the remainder being calcite and dolomite. The apatite is the hydroxy-fluor variety with low Sr, REE and Th. The origin of these ores is uncertain and is complicated by late-hydrothermal metasomatism which may have partially mobilized P. -R.A.H.",
author = "Bulakh, {A. G.} and Zolotarev, {A. A.} and Bobrova, {I. P.} and Gulii, {V. N.} and {Vande- Kirkov}, {Y. V.}",
year = "1984",
language = "русский",
volume = "113",
pages = "398--410",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "4",

}

RIS

TY - JOUR

T1 - (Mineralogy and genesis of the Seligdar apatite deposit (Aldan crystalline shield).

AU - Bulakh, A. G.

AU - Zolotarev, A. A.

AU - Bobrova, I. P.

AU - Gulii, V. N.

AU - Vande- Kirkov, Y. V.

PY - 1984

Y1 - 1984

N2 - Apatite-bearing rocks in this deposit in Precambrian gneisses and schists contain on average 18% apatite, the remainder being calcite and dolomite. The apatite is the hydroxy-fluor variety with low Sr, REE and Th. The origin of these ores is uncertain and is complicated by late-hydrothermal metasomatism which may have partially mobilized P. -R.A.H.

AB - Apatite-bearing rocks in this deposit in Precambrian gneisses and schists contain on average 18% apatite, the remainder being calcite and dolomite. The apatite is the hydroxy-fluor variety with low Sr, REE and Th. The origin of these ores is uncertain and is complicated by late-hydrothermal metasomatism which may have partially mobilized P. -R.A.H.

UR - http://www.scopus.com/inward/record.url?scp=0021567012&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0021567012

VL - 113

SP - 398

EP - 410

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 4

ER -

ID: 9332913