Plate‐Rate Frictional Behavior of Sediment Inputs to the Hikurangi Subduction Margin: How Does Lithology Control Slow Slip Events?
Abstract The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shallow (<15 km). The sedimentary sequence on the incoming plate is therefore representative of the shallow fault material where the SSEs will take place once they enter the subduction zone. K...
| الحاوية / القاعدة: | Geochemistry, Geophysics, Geosystems |
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| المؤلفون الرئيسيون: | , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Wiley
2022-06-01
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1029/2022GC010369 |