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Redistribution of material in the wall rock of a scheelite stockwork. / Panova, Y. G.; Barabanov, V. F.

In: Geochemistry International, Vol. 25, No. 12, 1988, p. 1-9.

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

Harvard

Panova, YG & Barabanov, VF 1988, 'Redistribution of material in the wall rock of a scheelite stockwork', Geochemistry International, vol. 25, no. 12, pp. 1-9.

APA

Panova, Y. G., & Barabanov, V. F. (1988). Redistribution of material in the wall rock of a scheelite stockwork. Geochemistry International, 25(12), 1-9.

Vancouver

Panova YG, Barabanov VF. Redistribution of material in the wall rock of a scheelite stockwork. Geochemistry International. 1988;25(12):1-9.

Author

Panova, Y. G. ; Barabanov, V. F. / Redistribution of material in the wall rock of a scheelite stockwork. In: Geochemistry International. 1988 ; Vol. 25, No. 12. pp. 1-9.

BibTeX

@article{2184a5b6054e485495f035a3c7105fd9,
title = "Redistribution of material in the wall rock of a scheelite stockwork",
abstract = "The mineral compositions of the veins and surrounding greisens in a scheelite stockwork have been examined, together with the behavior of petrogenetic, heavy, and rare elements. The rock-forming minerals vary in amount and composition as the vein contacts are approached, and this is accompanied by extensive element redistribution. It is concluded that the veins were produced by a metasomatic concretional mechanism. -Journal summary",
author = "Panova, {Y. G.} and Barabanov, {V. F.}",
year = "1988",
language = "English",
volume = "25",
pages = "1--9",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "12",

}

RIS

TY - JOUR

T1 - Redistribution of material in the wall rock of a scheelite stockwork

AU - Panova, Y. G.

AU - Barabanov, V. F.

PY - 1988

Y1 - 1988

N2 - The mineral compositions of the veins and surrounding greisens in a scheelite stockwork have been examined, together with the behavior of petrogenetic, heavy, and rare elements. The rock-forming minerals vary in amount and composition as the vein contacts are approached, and this is accompanied by extensive element redistribution. It is concluded that the veins were produced by a metasomatic concretional mechanism. -Journal summary

AB - The mineral compositions of the veins and surrounding greisens in a scheelite stockwork have been examined, together with the behavior of petrogenetic, heavy, and rare elements. The rock-forming minerals vary in amount and composition as the vein contacts are approached, and this is accompanied by extensive element redistribution. It is concluded that the veins were produced by a metasomatic concretional mechanism. -Journal summary

UR - http://www.scopus.com/inward/record.url?scp=0024220427&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0024220427

VL - 25

SP - 1

EP - 9

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 12

ER -

ID: 93226824