Grew E S, Manton W I
Science. 1979 Oct 26;206(4417):443-5. doi: 10.1126/science.206.4417.443.
Uranium-lead isotopic data indicate that the granulite-facies Napier complex of Enderby Land, Antarctica, was cut by charnockitic pegmatites 2.5 billion years ago and by pegmatites lacking hypersthene 0.52 billion years ago. The 4-bil-lion-years lead-lead ages (whole rock) reported for the Napier complex are rejected since these leads developed in three stages. Reconstructions of Gondwanaland suggest that the Napier complex may be a continuation of the Archean granulitic terrain of southern India.
铀铅同位素数据表明，南极洲恩德比地的麻粒岩相纳皮尔杂岩体在25亿年前被紫苏花岗岩伟晶岩切割，在5.2亿年前被不含紫苏辉石的伟晶岩切割。纳皮尔杂岩体报告的40亿年铅铅年龄（全岩）被否定，因为这些铅是分三个阶段形成的。冈瓦纳大陆的重建表明，纳皮尔杂岩体可能是印度南部太古宙麻粒岩地形的延续。
