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Plutonic mineral assemblages in Paleozoic dikes and explosion pipes of the alkaline province of the Baltic Shield. / Arzamastsev, A. A.; Dahlgren, S.

In: Geochemistry International, Vol. 31, No. 3, 01.01.1994, p. 57-68.

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@article{ea391fc87b964130a50a0e58c7eb78e4,
title = "Plutonic mineral assemblages in Paleozoic dikes and explosion pipes of the alkaline province of the Baltic Shield",
abstract = "Studies have been made of the barophile mineral phases making up mantle xenoliths and represented by xenocrysts in alkali picrites, damkjernites, melilitites, nephelinites, and kimberlites in explosion pipes and dikes from the surroundings of the Fen complex (Norway) and in the Kola peninsula. Based on the composition of the minerals and P-T estimates, conclusions are drawn on the heterogeneity of the mantle sources of dike magmatism during Paleozoic tectonic-magmatic reactivation. -from Journal summary",
author = "Arzamastsev, {A. A.} and S. Dahlgren",
year = "1994",
month = jan,
day = "1",
language = "English",
volume = "31",
pages = "57--68",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Plutonic mineral assemblages in Paleozoic dikes and explosion pipes of the alkaline province of the Baltic Shield

AU - Arzamastsev, A. A.

AU - Dahlgren, S.

PY - 1994/1/1

Y1 - 1994/1/1

N2 - Studies have been made of the barophile mineral phases making up mantle xenoliths and represented by xenocrysts in alkali picrites, damkjernites, melilitites, nephelinites, and kimberlites in explosion pipes and dikes from the surroundings of the Fen complex (Norway) and in the Kola peninsula. Based on the composition of the minerals and P-T estimates, conclusions are drawn on the heterogeneity of the mantle sources of dike magmatism during Paleozoic tectonic-magmatic reactivation. -from Journal summary

AB - Studies have been made of the barophile mineral phases making up mantle xenoliths and represented by xenocrysts in alkali picrites, damkjernites, melilitites, nephelinites, and kimberlites in explosion pipes and dikes from the surroundings of the Fen complex (Norway) and in the Kola peninsula. Based on the composition of the minerals and P-T estimates, conclusions are drawn on the heterogeneity of the mantle sources of dike magmatism during Paleozoic tectonic-magmatic reactivation. -from Journal summary

UR - http://www.scopus.com/inward/record.url?scp=0028257832&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0028257832

VL - 31

SP - 57

EP - 68

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 3

ER -

ID: 34786736