Refining the crust

doi:10.1038/s41561-025-01865-3

2025-12-08

PRE

Simon L. Harley *

DOI：10.1038/s41561-025-01865-3

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摘要

En 中文

像铀和钍这样的生热元素在岩石圈地壳下部亏损。地壳岩石的地球化学特征表明，需要极高的熔融温度才能造成这种亏损，并且可能还有助于稳定地壳。

Keyword:

crustal depletion

heat-producing elements

uranium

thorium

melting temperatures

期刊

Nature Geoscience

IF:

16.1

论文数:

4.6K

被引数:

4.1W

机构

University of Edinburgh

学者数:

5.2W

论文数: 4.6W

被引数: 71

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