岩板动力学与矿物相变期间的短暂弱化有关

IF 16.1 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2025-06-02 DOI:10.1038/s41561-025-01712-5

引用次数: 0

摘要

新的实验揭示了岩石变形和变质作用之间复杂的相互作用。地球地幔过渡带的板块停滞可以用橄榄石-尖晶石相变过程中的短暂减弱来解释。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Slab dynamics linked to transient weakening during mineral phase transitions

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Slab dynamics linked to transient weakening during mineral phase transitions

New experiments shed light on the complex interplay between rock deformation and metamorphism. Slab stagnation in Earth’s mantle transition zone may be explained by transient weakening during the olivine–spinel phase transition.

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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.