Data report: clay mineral assemblages within biocalcareous and volcaniclastic inputs to the Hikurangi subduction zone, IODP Expedition 372B/375 Sites U1520 and U1526, offshore New Zealand-Reference-Cited by-同舟云学术

Data report: clay mineral assemblages within biocalcareous and volcaniclastic inputs to the Hikurangi subduction zone, IODP Expedition 372B/375 Sites U1520 and U1526, offshore New Zealand

Published:2021-10-15 Issue: Volume: Page:
ISSN:2377-3189
Container-title:Hikurangi Subduction Margin Coring, Logging, and Observatories
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Author:

Underwood M.B.^ORCID

Publisher

International Ocean Discovery Program

Reference62 articles.

1. Slow slip source characterized by lithological and geometric heterogeneity

2. Site U1520

3. Mineralogy and Sedimentation of Recent Deep-Sea Clay in the Atlantic Ocean and Adjacent Seas and Oceans

4. Temperature-dependent frictional properties of heterogeneous Hikurangi Subduction Zone input sediments, ODP Site 1124

5. Evolution of the sedimentary system beneath the deep Pacific inflow off eastern New Zealand

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1. Volcanic ash alteration triggers active sedimentary lithium cycling: Insights from lithium isotopic compositions of pore fluids and sediments in the Hikurangi subduction zone;Earth and Planetary Science Letters;2024-09

2. Volcanic crustal structure of the western Hikurangi Plateau (New Zealand) from marine seismic reflection imaging;Geosphere;2024-04-25

3. Subducting volcaniclastic-rich upper crust supplies fluids for shallow megathrust and slow slip;Science Advances;2023-08-18

4. Ultralow frictional healing explains recurring slow slip events;Science;2023-02-17

5. Composition of fine‐grained sediment in the Hikurangi Trough: Evidence for intermingling among axial gravity flows, transverse gravity flows and margin‐parallel ocean currents;Sedimentology;2023-01-11