The origin of geochemical trends and Eoarchean (ca. 3700 Ma) zircons in Mesoarchean (ca. 3075 Ma) ocelli-hosting pillow basalts, Ivisaartoq greenstone belt, SW Greenland: evidence for crustal contamination versus crustal recycling.

A. Burak Polat; Robert Frei; B. Fryer; P W U Appel

The origin of geochemical trends and Eoarchean (ca. 3700 Ma) zircons in Mesoarchean (ca. 3075 Ma) ocelli-hosting pillow basalts, Ivisaartoq greenstone belt, SW Greenland: evidence for crustal contamination versus crustal recycling.

A. Burak Polat, Robert Frei, B. Fryer, P W U Appel

Geologi

28 Citationer (Scopus)

Originalsprog	Engelsk
Tidsskrift	Chemical Geology
Vol/bind	268
Sider (fra-til)	248-271
ISSN	0009-2541
Status	Udgivet - 2009

Citationsformater

The origin of geochemical trends and Eoarchean (ca. 3700 Ma) zircons in Mesoarchean (ca. 3075 Ma) ocelli-hosting pillow basalts, Ivisaartoq greenstone belt, SW Greenland: evidence for crustal contamination versus crustal recycling. / Polat, A. Burak; Frei, Robert; Fryer, B. et al.

I: Chemical Geology, Bind 268, 2009, s. 248-271.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › peer review

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AU - Polat, A. Burak

AU - Frei, Robert

AU - Fryer, B.

AU - Appel, P W U

PY - 2009

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M3 - Journal article

SN - 0009-2541

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JF - Chemical Geology

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