Discovery of the oldest oxic granitoids in the Kaapvaal Craton and its implications for the redox evolution of early Earth

Shunso Ishihara, Hiroshi Ohmoto, Carl R. Anhaeusser, Akira Imai, Laurence J. Robb

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Phanerozoic granitoids have been classified into magnetite and ilmenite series based on the abundance of magnetite, which is related to the Fe 2 O 3 /FeO ratio of the rock and the oxygen fugacity ( f O2 ) of its parent magma. We have examined the temporal and spatial distributions of both series in Archean granitoids from the Barberton region and the Johannesburg Dome of the Kaapvaal Craton, South Africa. The oldest syntectonic TTG (tonalite-trondhjemite-granodiorite) granitoids (ca. 3450 Ma in age) were found to be ilmenite series, whereas some intermediate-series granitoids occurred locally. Younger and larger syntectonic TTGs (e.g., the 3230 Ma Kaap Valley plutons) comprise nearly equal quantities of magnetite and ilmenite series. The major 3105 Ma calc-alkaline batholiths (e.g., Nelspruit batholith), emplaced during the late-tectonic stage, comprise mostly magnetite-series granitoids, suggesting that an oxidized continental crust already existed by this time. The rare earth element ratios and δ 18 O values, as well as the Fe 2 O 3 /FeO ratios, of the Archean magnetite-series granitoids suggest that their magmas were generated from the partial melting of subducted oceanic basalts that had been oxidized by interaction with seawater on mid-oceanic ridges; the processes of magma generation were much like those for Phanerozoic magnetite-series granitoids. This further suggests that the concentrations of oxidants (O 2 and/or SO 4 2- ) in the Archean oceans were similar to those in Phanerozoic oceans. Low concentrations of chlorine in the magmas, as well as deep levels of granite erosion, appear to explain the absence of major mineral deposits associated with the Kaapvaal granitoids.

Original languageEnglish
Pages (from-to)67-80
Number of pages14
JournalMemoir of the Geological Society of America
Volume198
DOIs
Publication statusPublished - Jan 1 2006

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early Earth
craton
magnetite
Phanerozoic
ilmenite
Archean
magma
trondhjemite
tonalite
ocean
mineral deposit
batholith
fugacity
granodiorite
oxidant
temporal distribution
continental crust
pluton
dome
partial melting

All Science Journal Classification (ASJC) codes

  • Geology

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Discovery of the oldest oxic granitoids in the Kaapvaal Craton and its implications for the redox evolution of early Earth. / Ishihara, Shunso; Ohmoto, Hiroshi; Anhaeusser, Carl R.; Imai, Akira; Robb, Laurence J.

In: Memoir of the Geological Society of America, Vol. 198, 01.01.2006, p. 67-80.

Research output: Contribution to journalArticle

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