1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment

UB Andersson; Olav Eklund; Sören Fröjdö; D Konopelko

doi:10.1016/j.lithos.2005.04.001

1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment

UB Andersson, Olav Eklund, Sören Fröjdö, D Konopelko

Tutkimustuotos: Lehtiartikkeli › Artikkeli › Tieteellinen › vertaisarvioitu

65 Sitaatiot (Scopus)

Abstrakti

A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved.

Alkuperäiskieli	Ei tiedossa
Sivut	110–136
Sivumäärä	27
Julkaisu	Lithos
Vuosikerta	86
Numero	1-2
DOI - pysyväislinkit	https://doi.org/10.1016/j.lithos.2005.04.001
Tila	Julkaistu - 2006
OKM-julkaisutyyppi	A1 Julkaistu artikkeli, soviteltu

Keywords

1.8 Ga mafic magmatism
carbonate metasomatism
mantle enrichment
Nd-Sr isotopes
Fennoscandian Shield

Pääsy asiakirjaan

10.1016/j.lithos.2005.04.001

Viittausmuodot

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title = "1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment",

abstract = "A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved.",

keywords = "1.8 Ga mafic magmatism, carbonate metasomatism, mantle enrichment, Nd-Sr isotopes, Fennoscandian Shield, 1.8 Ga mafic magmatism, carbonate metasomatism, mantle enrichment, Nd-Sr isotopes, Fennoscandian Shield, 1.8 Ga mafic magmatism, carbonate metasomatism, mantle enrichment, Nd-Sr isotopes, Fennoscandian Shield",

author = "UB Andersson and Olav Eklund and S{\"o}ren Fr{\"o}jd{\"o} and D Konopelko",

year = "2006",

doi = "10.1016/j.lithos.2005.04.001",

language = "Odefinierat/ok{\"a}nt",

volume = "86",

pages = "110–136",

journal = "Lithos",

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TY - JOUR

T1 - 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment

AU - Andersson, UB

AU - Eklund, Olav

AU - Fröjdö, Sören

AU - Konopelko, D

PY - 2006

Y1 - 2006

N2 - A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved.

AB - A convergent continental margin setting with transpressional shearing was active during TIB formation in the west. Whether this shearing was instrumental in the formation of the 1.8 Ga magmatism further continentwards, or if the magmatisin in the central and eastern areas was the result of extensional collapse or plume activity is presently not known. (c) 2005 Elsevier B.V. All rights reserved.

KW - 1.8 Ga mafic magmatism

KW - carbonate metasomatism

KW - mantle enrichment

KW - Nd-Sr isotopes

KW - Fennoscandian Shield

KW - 1.8 Ga mafic magmatism

KW - carbonate metasomatism

KW - mantle enrichment

KW - Nd-Sr isotopes

KW - Fennoscandian Shield

KW - 1.8 Ga mafic magmatism

KW - carbonate metasomatism

KW - mantle enrichment

KW - Nd-Sr isotopes

KW - Fennoscandian Shield

U2 - 10.1016/j.lithos.2005.04.001

DO - 10.1016/j.lithos.2005.04.001

M3 - Artikel

SN - 0024-4937

VL - 86

SP - 110

EP - 136

JO - Lithos

JF - Lithos

IS - 1-2

ER -