Application of a Premelting Model to the Lithosphere‐Asthenosphere Boundary
Abstract A seismic discontinuity known as the G‐discontinuity, which has been prevailingly detected in the oceanic mantle, is considered to provide evidence of a sharp lithosphere‐asthenosphere boundary (LAB). We investigate whether this sharp LAB is explained by grain boundary premelting, which cau...
محفوظ في:
| المؤلفون الرئيسيون: | , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
Wiley
2020-11-01
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| سلاسل: | Geochemistry, Geophysics, Geosystems |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1029/2020GC009338 |
| الوسوم: |
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