Evidence for Extremely Rapid (sub-Myr Timescales) UHT Metamorphic Sole Formation during Spontaneous Subduction Initiation in Nagaland – Manipur ophiolite belt, Indo-Myanmar Ranges [PDF]
Santanu Kumar Bhowmik +4 more
openalex +1 more source
Dataset for "continental tip is a favorable location for subduction initiation"
Shengxing Zhang
openalex +1 more source
Forearc Ophiolites: Archives of Subduction Initiation and Melt Evolution in Convergent Margin Settings [PDF]
Yıldırım Dilek
openalex +1 more source
Correction to “Newtonian versus non‐Newtonian upper mantle viscosity: Implications for subduction initiation” [PDF]
M. I. Billen, Greg Hirth
openalex +1 more source
Seismicity and Ground Motion Simulations of the SW Iberia Margin [PDF]
In this study, we focus on the region between Gorringe Bank and the Horseshoe Fault located in the SW Iberia margin, which is believed to be the site of the great 1755 earthquake.
Bezzeghoud, M. +2 more
core
Geodetic Observations of Weak Determinism in Rupture Evolution of Large Earthquakes. [PDF]
The moment evolution of large earthquakes is a subject of fundamental interest to both basic and applied seismology. Specifically, an open problem is when in the rupture process a large earthquake exhibits features dissimilar from those of a lesser ...
Allen, RM +3 more
core
Origin of Philippine Sea Basins During Subduction Initiation in the Western Pacific
Understanding the age and dynamics of the overriding plates allows an assessment of competing subduction initiation hypotheses. The Izu‐Bonin‐Mariana margin in the Western Pacific is a key example of initiation and hence it is important to constrain the ...
Osamu Ishizuka +16 more
doaj +1 more source
Loess Studies in Aotearoa New Zealand
Loess in Aotearoa New Zealand (ANZ) has been studied since its first documented recognition (on Banks Peninsula) in 1878 by Julius von Haast. A decade later, John Hardcastle revealed that southern ANZ loess was both glacial in origin and contained signals of past climates.
Brent V. Alloway +4 more
wiley +1 more source

