How Clay Mineral Assemblages Affect Instability on the Upper Slope of the Hikurangi Subduction Zone, New Zealand

Abstract The International Ocean Discovery Program cored Sites U1517 (Tuaheni landslide) and U1519 (Tuaheni Basin) on the Hikurangi slope, North Island, New Zealand. We employed X‐ray diffraction to document clay mineral assemblages within the muddy sediments, with the aim of testing their potential...

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Principais autores:	Michael B. Underwood, Brandon Dugan, Sebastian Cardona
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2022-11-01
coleção:	Geophysical Research Letters
Assuntos:	International Ocean Discovery Program Hikurangi subduction zone New Zealand trench slope sediments clay mineral assemblages submarine landslide
Acesso em linha:	https://doi.org/10.1029/2022GL100529
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