哈代人
镁铁质
地质学
放射性核素
火成岩
地质年代学
结壳
太古宙
地球化学
大陆地壳
地幔(地质学)
作者
Christian Sole,Jonathan OʼNeil,Hanika Rizo,Jean‐Louis Paquette,D.J.A. Evans and D.I. Benn,J. Plakholm
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2025-06-26
卷期号:388 (6754): 1431-1435
被引量:17
标识
DOI:10.1126/science.ads8461
摘要
Many questions remain regarding Earth's earliest crust owing to the rarity of Hadean (>4.03 billion-year-old) rocks and minerals. The Nuvvuagittuq Greenstone Belt (NGB) in Canada may be the only known remnant of Hadean crust, although its age is debated, ranging from ≥3.75 to 4.3 billion years old. Mafic intrusions within this belt were specifically sampled and analyzed to investigate the timing of their magmatic differentiation. Correlations between samarium/neodymium (Sm/Nd) and 143Nd/144Nd and 142Nd/144Nd ratios correspond to ages of 4157 ± 174 and [Formula: see text] million years for the long-lived 147Sm-143Nd and the short-lived 146Sm-142Nd systems, respectively. The age agreement between both extant and extinct radiogenic systems, in rocks related through igneous fractionation, is compelling evidence for preservation of Hadean rocks in the NGB, opening a rare window into Earth's earliest times.
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