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Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East). / Krivovichev, V.G.; Brusnitsyn, A.I.; Zaitsev, A.N.

In: Geochemistry International, Vol. 34, No. 2, 1996, p. 91-96.

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

Harvard

Krivovichev, VG, Brusnitsyn, AI & Zaitsev, AN 1996, 'Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East)', Geochemistry International, vol. 34, no. 2, pp. 91-96.

APA

Krivovichev, V. G., Brusnitsyn, A. I., & Zaitsev, A. N. (1996). Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East). Geochemistry International, 34(2), 91-96.

Vancouver

Krivovichev VG, Brusnitsyn AI, Zaitsev AN. Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East). Geochemistry International. 1996;34(2):91-96.

Author

Krivovichev, V.G. ; Brusnitsyn, A.I. ; Zaitsev, A.N. / Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East). In: Geochemistry International. 1996 ; Vol. 34, No. 2. pp. 91-96.

BibTeX

@article{e71b7d2c633840409a509719f7608ad3,
title = "Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East)",
abstract = "A radiometric age of 83.4 ±3.2 Ma and initial 87Sr/86Sr of 0.75058 ±0.00068, indicative of sialic matter melting in the upper or middle crust, were established by the Rb-Sr method for the Verkhneurmi massif granite. From the early to the late emplacement phases, the granite is shown to become progressively enriched in Na + K, Li, Rb, Cs, Nb, Y, Yb, W, Sn, and F, and depleted in Ti, Fe, Mg, Ca, Ba, Sr, and Mo. Significant correlations were established between the alumina coefficient [Al2O3/(FeO + Fe2O3 + MgO)], total alkali content (Na2O + K2O), and fractionation degree of the granite [lg (Rb/Ba)]. The most differentiated rock of the massif is the Li-F-leucogranite, which is the likely source of the fluids responsible for metasomatic reworking of rhyolite and granite to produce the Sn-bearing quartz-topaz-siderophyllite greisen of the Pravourmi deposit.",
author = "V.G. Krivovichev and A.I. Brusnitsyn and A.N. Zaitsev",
note = "RADIOMETRIC AGE AND GEOCHEMISTRY OF THE VERKHNEURMI MASSIF GRANITE (THE AMUR REGION, FAR EAST) KRIVOVICHEV V.G.*1, BRUSNITSYN A.I.1, ZAITSEV A.N.1 1 Geological Faculty, St. Petersburg State University, Universitetskaya nab. 7/9 Тип: статья в журнале - научная статья Язык: английский Том: 34Номер: 2 Год: 1996 Страницы: 91-96 ЖУРНАЛ: GEOCHEMISTRY INTERNATIONAL Издательство: Pleiades Publishing, Ltd. (Плеадес Паблишинг, Лтд) (Род-Таун) ISSN: 0016-7029eISSN: 1531-8397 ",
year = "1996",
language = "English",
volume = "34",
pages = "91--96",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Radiometric age and geochemistry of the Verkhneurmi massif granite (the Amur region, Far East)

AU - Krivovichev, V.G.

AU - Brusnitsyn, A.I.

AU - Zaitsev, A.N.

N1 - RADIOMETRIC AGE AND GEOCHEMISTRY OF THE VERKHNEURMI MASSIF GRANITE (THE AMUR REGION, FAR EAST) KRIVOVICHEV V.G.*1, BRUSNITSYN A.I.1, ZAITSEV A.N.1 1 Geological Faculty, St. Petersburg State University, Universitetskaya nab. 7/9 Тип: статья в журнале - научная статья Язык: английский Том: 34Номер: 2 Год: 1996 Страницы: 91-96 ЖУРНАЛ: GEOCHEMISTRY INTERNATIONAL Издательство: Pleiades Publishing, Ltd. (Плеадес Паблишинг, Лтд) (Род-Таун) ISSN: 0016-7029eISSN: 1531-8397

PY - 1996

Y1 - 1996

N2 - A radiometric age of 83.4 ±3.2 Ma and initial 87Sr/86Sr of 0.75058 ±0.00068, indicative of sialic matter melting in the upper or middle crust, were established by the Rb-Sr method for the Verkhneurmi massif granite. From the early to the late emplacement phases, the granite is shown to become progressively enriched in Na + K, Li, Rb, Cs, Nb, Y, Yb, W, Sn, and F, and depleted in Ti, Fe, Mg, Ca, Ba, Sr, and Mo. Significant correlations were established between the alumina coefficient [Al2O3/(FeO + Fe2O3 + MgO)], total alkali content (Na2O + K2O), and fractionation degree of the granite [lg (Rb/Ba)]. The most differentiated rock of the massif is the Li-F-leucogranite, which is the likely source of the fluids responsible for metasomatic reworking of rhyolite and granite to produce the Sn-bearing quartz-topaz-siderophyllite greisen of the Pravourmi deposit.

AB - A radiometric age of 83.4 ±3.2 Ma and initial 87Sr/86Sr of 0.75058 ±0.00068, indicative of sialic matter melting in the upper or middle crust, were established by the Rb-Sr method for the Verkhneurmi massif granite. From the early to the late emplacement phases, the granite is shown to become progressively enriched in Na + K, Li, Rb, Cs, Nb, Y, Yb, W, Sn, and F, and depleted in Ti, Fe, Mg, Ca, Ba, Sr, and Mo. Significant correlations were established between the alumina coefficient [Al2O3/(FeO + Fe2O3 + MgO)], total alkali content (Na2O + K2O), and fractionation degree of the granite [lg (Rb/Ba)]. The most differentiated rock of the massif is the Li-F-leucogranite, which is the likely source of the fluids responsible for metasomatic reworking of rhyolite and granite to produce the Sn-bearing quartz-topaz-siderophyllite greisen of the Pravourmi deposit.

M3 - Article

VL - 34

SP - 91

EP - 96

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 2

ER -

ID: 5034091