Comment on "A Vestige of Earth's Oldest Ophiolite"-Reference-Cited by-同舟云学术

Comment on "A Vestige of Earth's Oldest Ophiolite"

Published:2007-11-02 Issue:5851 Volume:318 Page:746-746
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Nutman Allen P.¹²,Friend Clark R. L.¹²

Affiliation:

1. Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China.

2. 45 Stanway Road, Headington, Oxford OX3 8HU, UK.

Abstract

Furnes et al . (Reports, 23 March 2007, p. 1704) reported the identification of an ophiolite sequence within the ∼3.8-billion-year-old Isua supracrustal belt. However, they did not acknowledge that the belt contains supracrustal rocks and mafic dikes of different ages, nor did they demonstrate that the proposed components of the ophiolite are coeval.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference8 articles.

1. A Vestige of Earth's Oldest Ophiolite

2. ∼ 3710 and ⪖ 3790 Ma volcanic sequences in the Isua (Greenland) supracrustal belt; structural and Nd isotope implications

3. Dating of the Ameralik dyke swarms of the Nuuk district, southern West Greenland: mafic intrusion events starting fromc. 3510 Ma

4. Geochem. Geophys. Geosyst. 2001 2

5. J. H. Allaart, in The Early History of the Earth, B. F. Windley, Ed. (Wiley, London, 1976), pp. 177–189.

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