Nutman Allen P, Friend Clark R L
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China.
Science. 2007 Nov 2;318(5851):746. doi: 10.1126/science.1144148.
Furnes et al. (Reports, 23 March 2007, p. 1704) reported the identification of an ophiolite sequence within the approximately 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.
弗内斯等人（《报告》，2007年3月23日，第1704页）报告了在约38亿年前的伊苏阿上地壳带内发现了一个蛇绿岩序列。然而，他们没有承认该地带包含不同年龄的上地壳岩石和镁铁质岩脉，也没有证明所提出的蛇绿岩成分是同时期的。
