How Clay Mineral Assemblages Affect Instability on the Upper Slope of the Hikurangi Subduction Zone, New Zealand-Reference-Cited by-同舟云学术

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

Published:2022-11-09 Issue:21 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Underwood Michael B.¹^ORCID,Dugan Brandon²^ORCID,Cardona Sebastian³

Affiliation:

1. Department of Earth and Environmental Science New Mexico Institute of Mining and Technology Socorro NM USA

2. Department of Geophysics and Hydrologic Science and Engineering Program Colorado School of Mines Golden CO USA

3. Department of Geology and Geophysics Texas A&M University College Station TX USA

Funder

United States Science Support Program

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL100529

Reference127 articles.

1. New constraints on oceanographic vs. seismic control on submarine landslide initiation: a geotechnical approach off Uruguay and northern Argentina

2. Modern sediment dispersal and accumulation on the outer Poverty continental margin

3. Contourite vs gravity-flow deposits of the Pleistocene Faro Drift (Gulf of Cadiz): Sedimentological and mineralogical approaches

4. Sealing potential of contourite drifts in deep-water fold and thrust belts: Examples from the Hikurangi Margin, New Zealand

5. Distribution of contourite drifts on convergent margins: Examples from the Hikurangi subduction margin of New Zealand

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