Early start to volatile cycling

IF 15.7 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2025-04-18 DOI:10.1038/s41561-025-01689-1

J. Elis Hoffmann

引用次数: 0

Abstract

Ancient metamorphosed basalts show a sulfur isotopic fingerprint of surface sediment, suggesting volatile cycling by a subduction-like process was occurring more than 3.8 billion years ago.

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前期开始波动循环

古代变质玄武岩显示出地表沉积物的硫同位素指纹，表明通过类似俯冲过程的挥发性循环发生在38亿年前。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Nature Geoscience 地学-地球科学综合

CiteScore

26.70

自引率

1.60%

发文量

187

审稿时长

3.3 months

期刊介绍： Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.