A thin mantle transition zone beneath the equatorial Mid-Atlantic Ridge
The location and degree of material transfer between the upper and lower mantle are key to Earth’s thermal and chemical evolution. Sinking slabs and rising plumes are generally accepted as locations of transfer, whereas mid-ocean ridges are not typically assumed to play a role. However, tight constr...
| المؤلفون الرئيسيون: | , , , , |
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| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
Springer Nature
2021
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