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Journal ArticleDOI

Age significance of U-Th-Pb zircon data from early Archaean rocks of west Greenland - a reassessment based on combined ion-microprobe and imaging studies - reply

TLDR
In this paper, the geochronological evolution of early Archaean gneisses from southern West Greenland is reassessed using the well-established cathodoluminescence imaging method both to reveal previously undocumented complex zircon growth histories and to control positioning of ion-microprobe U-Th-Pb analyses.
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This article is published in Chemical Geology.The article was published on 1999-08-10. It has received 516 citations till now. The article focuses on the topics: Zircon & Akilia.

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Journal ArticleDOI

Atlas of Zircon Textures

TL;DR: In this paper, a selection of both the most typical, but also of the less common, features seen in zircon, categorized according to the different geological processes responsible for their formation are presented.
Journal ArticleDOI

Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization

TL;DR: In this article, a new generation of large radius magnetic sector multicollector Cameca IMS-1280 SIMS was used to date Phanerozoic zircons.
Journal ArticleDOI

Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution

TL;DR: In this article, an integrated approach is explored with new data from the Lachlan Fold Belt in south-east Australia. And the results show that the ages of zircons with high δ18O values (greater than 6.5‰) peak at about 1.8-2.0 Ga.
Journal ArticleDOI

The generation and evolution of the continental crust

TL;DR: The continental crust is the archive of the geological history of the Earth and only 7% of the crust is older than 2.5 Ga, and yet significantly more crust was generated before than subsequently.
References
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Approximation of terrestrial lead isotope evolution by a two-stage model

TL;DR: In this paper, a two-stage model for terrestrial lead isotope evolution is proposed, which permits the age of the earth to be that of the meteorite system and also yields good model ages for samples of all ages.
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Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types

TL;DR: In this article, the saturation behavior of zircon in crustal anatectic melts as a function of both temperature and composition has been studied and a model of Zr solubility given by: In D Zr Zircon/melt = −3.80−[0.85(M−1)]+12900/T where T is the absolute temperature, and M is the cation ratio (Na + K + 2Ca)/(Al · Si).
Journal ArticleDOI

Evidence for life on Earth before 3,800 million years ago.

TL;DR: In this article, ion-microprobe measurements of the carbon-isotope composition of carbonaceous inclusions within grains of apatite (basic calcium phosphate) from the oldest known sediment sequences a approx. 3,800 Myr-old banded iron formation from the Isua supracrustal belt, West Greenland and a similar formation from Akilia island that is possibly older than 3,850 Myr.
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Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides: II. Ion microprobe zircon U-Th-Pb

TL;DR: In this article, an ion microprobe U-Th-Pb analysis of residual cores and metamorphic mantles of zircons from three high grade paragneisses from the Seve Nappe Complex, north-western Sweden, showed that the sediments comprising the protolith of the gneisses over a distance of 250 km were probably derived from similarly-aged source terranes.
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