Standard

(Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan). / Zolotarev, A. A.; Bobrova, I. P.; Bulakh, A. G.

In: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, Vol. 112, No. 3, 1983, p. 325-333.

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

Harvard

Zolotarev, AA, Bobrova, IP & Bulakh, AG 1983, '(Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan).', Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, vol. 112, no. 3, pp. 325-333.

APA

Zolotarev, A. A., Bobrova, I. P., & Bulakh, A. G. (1983). (Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, 112(3), 325-333.

Vancouver

Zolotarev AA, Bobrova IP, Bulakh AG. (Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1983;112(3):325-333.

Author

Zolotarev, A. A. ; Bobrova, I. P. ; Bulakh, A. G. / (Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan). In: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1983 ; Vol. 112, No. 3. pp. 325-333.

BibTeX

@article{b326402be45d42b2b1226be1576b6236,
title = "(Mineralogy and features of the genesis of apatite-{"}forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan).",
abstract = "Two types of apatite-forsterite-carbonate rocks occur in this SE Yakutian deposit: those in which the dominant carbonate is calcite and those in which it is dolomite. Medium-grained stratiform bodies contain serpentine, talc, apatite, carbonate and magnetite as the major minerals, the serpentine and talc being pseudomorphous after olivine. Apatite has the composition SiO2 1.65, TiO2 0.006, Al2O3 0.09, Fe2O3 0.54, FeO 0.12, CaO 54.69, MgO 0.64, MnO 0.01, SrO 0.20, Na2O 0.14, K2O 0.02, ThO2 0.01, TR2O3 0.27, P2O5 41.10, H2O+ 0.34, H2O- 0.35, F 2.75, (=102.926); epsilon 1.632-1.634, omega 1.635-1.637; D 3.15 g/cm3; a 9.388, c 6.889 A. These rocks were formed by the metamorphism and metasomatism of forsteritic limestones at 700o-500oC.-R.A.H.",
author = "Zolotarev, {A. A.} and Bobrova, {I. P.} and Bulakh, {A. G.}",
year = "1983",
language = "русский",
volume = "112",
pages = "325--333",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "3",

}

RIS

TY - JOUR

T1 - (Mineralogy and features of the genesis of apatite-"forsterite'- carbonate rocks of the Seligdarskoe deposit (Aldan).

AU - Zolotarev, A. A.

AU - Bobrova, I. P.

AU - Bulakh, A. G.

PY - 1983

Y1 - 1983

N2 - Two types of apatite-forsterite-carbonate rocks occur in this SE Yakutian deposit: those in which the dominant carbonate is calcite and those in which it is dolomite. Medium-grained stratiform bodies contain serpentine, talc, apatite, carbonate and magnetite as the major minerals, the serpentine and talc being pseudomorphous after olivine. Apatite has the composition SiO2 1.65, TiO2 0.006, Al2O3 0.09, Fe2O3 0.54, FeO 0.12, CaO 54.69, MgO 0.64, MnO 0.01, SrO 0.20, Na2O 0.14, K2O 0.02, ThO2 0.01, TR2O3 0.27, P2O5 41.10, H2O+ 0.34, H2O- 0.35, F 2.75, (=102.926); epsilon 1.632-1.634, omega 1.635-1.637; D 3.15 g/cm3; a 9.388, c 6.889 A. These rocks were formed by the metamorphism and metasomatism of forsteritic limestones at 700o-500oC.-R.A.H.

AB - Two types of apatite-forsterite-carbonate rocks occur in this SE Yakutian deposit: those in which the dominant carbonate is calcite and those in which it is dolomite. Medium-grained stratiform bodies contain serpentine, talc, apatite, carbonate and magnetite as the major minerals, the serpentine and talc being pseudomorphous after olivine. Apatite has the composition SiO2 1.65, TiO2 0.006, Al2O3 0.09, Fe2O3 0.54, FeO 0.12, CaO 54.69, MgO 0.64, MnO 0.01, SrO 0.20, Na2O 0.14, K2O 0.02, ThO2 0.01, TR2O3 0.27, P2O5 41.10, H2O+ 0.34, H2O- 0.35, F 2.75, (=102.926); epsilon 1.632-1.634, omega 1.635-1.637; D 3.15 g/cm3; a 9.388, c 6.889 A. These rocks were formed by the metamorphism and metasomatism of forsteritic limestones at 700o-500oC.-R.A.H.

UR - http://www.scopus.com/inward/record.url?scp=0021044390&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0021044390

VL - 112

SP - 325

EP - 333

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 3

ER -

ID: 9333043