Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition

A. Polat; A.W. Hofmann; P.W.U. Appel

doi:10.1016/S0166-2635(04)80004-5

Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition

A. Polat, A.W. Hofmann, P.W.U. Appel

Afdeling for Kortlægning og Mineralske Råstoffer

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

2 Citationer (Scopus)

Resumé

Geochemical signatures in Archaean mafic to ultramafic volcanic rocks can provide important constraints on the thermal and chemical characteristics of their mantle source regions.

Originalsprog	Engelsk
Titel	The Precambrian Earth
Undertitel	Tempos and Events
Redaktører	P.G. Eriksson, W. Altermann, D.R. Nelson, W.U. Mueller, O. Catunecanu
Forlag	Elsevier
Sider	74-88
Antal sider	15
ISBN (Trykt)	978-0-444-51506-3
DOI	https://doi.org/10.1016/S0166-2635(04)80004-5
Status	Udgivet - 2004

Publikationsserier

Navn	Developments in Precambrian Geology
Vol/bind	12
ISSN	0166-2635

Programområde

Programområde 4: Mineralske råstoffer

Adgang til dokumentet

10.1016/S0166-2635(04)80004-5

Citationsformater

Polat, A., Hofmann, A. W., & Appel, P. W. U. (2004). Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition. I P. G. Eriksson, W. Altermann, D. R. Nelson, W. U. Mueller, & O. Catunecanu (red.), The Precambrian Earth: Tempos and Events (s. 74-88). Elsevier. https://doi.org/10.1016/S0166-2635(04)80004-5

Polat, A. ; Hofmann, A.W. ; Appel, P.W.U. / Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition. The Precambrian Earth: Tempos and Events. red. / P.G. Eriksson ; W. Altermann ; D.R. Nelson ; W.U. Mueller ; O. Catunecanu. Elsevier, 2004. s. 74-88 (Developments in Precambrian Geology, Bind 12).

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abstract = "Geochemical signatures in Archaean mafic to ultramafic volcanic rocks can provide important constraints on the thermal and chemical characteristics of their mantle source regions.",

author = "A. Polat and A.W. Hofmann and P.W.U. Appel",

year = "2004",

doi = "10.1016/S0166-2635(04)80004-5",

language = "English",

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Polat, A, Hofmann, AW & Appel, PWU 2004, Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition. i PG Eriksson, W Altermann, DR Nelson, WU Mueller & O Catunecanu (red), The Precambrian Earth: Tempos and Events. Elsevier, Developments in Precambrian Geology, bind 12, s. 74-88. https://doi.org/10.1016/S0166-2635(04)80004-5

Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition. / Polat, A.; Hofmann, A.W.; Appel, P.W.U.
The Precambrian Earth: Tempos and Events. red. / P.G. Eriksson; W. Altermann; D.R. Nelson; W.U. Mueller; O. Catunecanu. Elsevier, 2004. s. 74-88 (Developments in Precambrian Geology, Bind 12).

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

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AU - Polat, A.

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PY - 2004

Y1 - 2004

N2 - Geochemical signatures in Archaean mafic to ultramafic volcanic rocks can provide important constraints on the thermal and chemical characteristics of their mantle source regions.

AB - Geochemical signatures in Archaean mafic to ultramafic volcanic rocks can provide important constraints on the thermal and chemical characteristics of their mantle source regions.

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T3 - Developments in Precambrian Geology

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Polat A, Hofmann AW, Appel PWU. Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition. I Eriksson PG, Altermann W, Nelson DR, Mueller WU, Catunecanu O, red., The Precambrian Earth: Tempos and Events. Elsevier. 2004. s. 74-88. (Developments in Precambrian Geology, Bind 12). doi: 10.1016/S0166-2635(04)80004-5

Geochemical diversity in volcanic rocks of the > 3.7-3.8 Ga Isua greenstone belt, SW Greenland: Implications for Mantle Composition

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