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...

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Hlavní autoři: Jade Dutilleul, S. Bourlange, Y. Géraud
Médium: Článek
Jazyk:English
Vydáno: Wiley 2021-10-01
Edice:Geochemistry, Geophysics, Geosystems
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On-line přístup:https://doi.org/10.1029/2020GC009325