Porosity and Compaction State at the Active Pāpaku Thrust Fault in the Frontal Accretionary Wedge of the North Hikurangi Margin
Abstract Characterization of the porosity evolution across the sedimentary section entering subduction zones and accreted sediments provide valuable information for understanding the deformation history at accretionary margins and the physico‐chemical processes in and around fault zones. Internation...
| Egile Nagusiak: | , , |
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| Formatua: | Artikulua |
| Hizkuntza: | English |
| Argitaratua: |
Wiley
2021-10-01
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| Saila: | Geochemistry, Geophysics, Geosystems |
| Gaiak: | |
| Sarrera elektronikoa: | https://doi.org/10.1029/2020GC009325 |