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

Geology

28 Citations (Scopus)

Original language	English
Journal	Chemical Geology
Volume	268
Pages (from-to)	248-271
ISSN	0009-2541
Publication status	Published - 2009

Cite this

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.

In: Chemical Geology, Vol. 268, 2009, p. 248-271.

Research output: Contribution to journal › Journal article › Research › peer-review

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title = "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.",

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AU - Polat, A. Burak

AU - Frei, Robert

AU - Fryer, B.

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