Amanote Research
Register
Sign In
Discover open access scientific publications
Search, annotate, share and cite publications
Publications by Shipboard Scientists
Structural Analysis of Compactive Deformation in the Incoming Sedimentary Section of the Hikurangi Subduction Margin, New Zealand: Results From IODP 375 Expedition
Acta Geologica Sinica
Geology
Related publications
The Giant Ruatoria Debris Avalanche on the Northern Hikurangi Margin, New Zealand: Result of Oblique Seamount Subduction
Journal of Geophysical Research
Geochemistry
Space
Planetary Sciences
Oceanography
Paleontology
Petrology
Soil Science
Forestry
Atmospheric Science
Ecology
Geophysics
Aquatic Science
Earth
Earth-Surface Processes
Planetary Science
Technology
Water Science
IODP Expedition 317: Exploring the Record of Sea-Level Change Off New Zealand
Scientific Drilling
Power Technology
Mechanical Engineering
Energy Engineering
Subducted Seamount Diverts Shallow Slow Slip to the Forearc of the Northern Hikurangi Subduction Zone, New Zealand
Geology
Geology
The New Zealand Antarctic Expedition
Nature
Multidisciplinary
Data Report: Stable Isotope Composition of Authigenic Carbonates From the Northern Cascadia Margin, IODP Expedition 311, Sites U1325-U1329
Proceedings of the IODP
Active Venting Sites on the Gas-Hydrate-Bearing Hikurangi Margin, Off New Zealand: Diffusive- Versus Bubble-Released Methane
Marine Geology
Petrology
Geochemistry
Oceanography
Geology
Hydrogeological Responses to Incoming Materials at the Erosional Subduction Margin, Offshore Osa Peninsula, Costa Rica
Geochemistry, Geophysics, Geosystems
Petrology
Geochemistry
Geophysics
Continental Margin Deformation Along the Andean Subduction Zone: Thermo-Mechanical Models
Physics of the Earth and Planetary Interiors
Planetary Science
Space
Geophysics
Astrophysics
Astronomy
Physics
Data Report: Multiscale Visualization of Stylolites, Deformations in Chalk From Subunit IIIB, Site U1480, IODP Expedition 362, Sumatra Subduction Zone
Proceedings of the International Ocean Discovery Program
