Sulfide resorption during crustal ascent and degassing of oceanic plateau basalts [PDF]
The solubility of sulfur in basaltic melt has important implications for the formation of magmatic ore deposits. Here, the authors show that magma ascent and sulfur-degassing influence the degree to which basaltic magmas are enriched in economically ...
C. D. J. Reekie +5 more
doaj +2 more sources
Probing the world's largest oceanic plateau: from making to collision. [PDF]
The enormously thick Ontong Java Plateau crust was built primarily by deep magma intrusion and underplating, with relatively minor contribution from flood basalts.
Jiang X +6 more
europepmc +3 more sources
The seismic Moho structure of Shatsky Rise oceanic plateau, northwest Pacific Ocean [PDF]
Abstract Oceanic plateaus are large igneous provinces formed by extraordinary eruptions that create thick oceanic crust, whose structure is poorly known owing to the lack of deep-penetration seismic data. Multichannel seismic (MCS) reflection and wide-angle refraction data allow us to show Moho structure beneath a large part of the Shatsky Rise ...
Jinchang Zhang, Jun Korenaga
exaly +2 more sources
The architecture of oceanic plateaus revealed by the volcanic stratigraphy of the accreted Wrangellia oceanic plateau [PDF]
The accreted Wrangellia flood basalts and associated sedimentary rocks that compose the prevolcanic and postvolcanic stratigraphy provide an unparalleled view of the architecture, eruptive environment, and accumulation and subsidence history of an oceanic plateau.
Andrew R. Greene +5 more
openaire +2 more sources
Petrogenesis of Siletzia: The world's youngest oceanic plateau [PDF]
Siletzia is an accreted Palaeocene-Eocene Large Igneous Province, preserved in the northwest United States and southern Vancouver Island. Although previous workers have suggested that components of Siletzia were formed in tectonic settings including back arc basins, island arcs and ocean islands, more recent work has presented evidence for parts of ...
Ciborowski, T. Jake R. +4 more
openaire +1 more source
Mesozooplankton structure and functioning during the onset of the Kerguelen phytoplankton bloom during the KEOPS2 survey [PDF]
This paper presents results on the spatial and temporal distribution patterns of mesozooplankton in the naturally fertilized region to the east of the Kerguelen Islands (Southern Ocean) visited at early bloom stage during the KEOPS2 survey (15 October to
F. Carlotti +7 more
doaj +1 more source
Valdivia Bank (VB) is a Late Cretaceous oceanic plateau formed by volcanism from the Tristan‐Gough hotspot at the Mid‐Atlantic Ridge (MAR). To better understand its origin and evolution, magnetic data were used to generate a magnetic anomaly grid, which ...
S. Thoram +29 more
doaj +1 more source
Aseismic ridge subduction and flat subduction: Insights from three-dimensional numerical models
Flat subduction can significantly influence the distribution of volcanism, stress state, and surface topography of the overriding plate. However, the mechanisms for inducing flat subduction remain controversial.
Hui Zhao, Wei Leng
doaj +1 more source
Rifting of the oceanic Azores Plateau with episodic volcanic activity [PDF]
AbstractExtension of the Azores Plateau along the Terceira Rift exposes a lava sequence on the steep northern flank of the Hirondelle Basin. Unlike typical tholeiitic basalts of oceanic plateaus, the 1.2 km vertical submarine stratigraphic profile reveals two successive compositionally distinct basanitic to alkali basaltic eruptive units.
Storch, B. +4 more
openaire +2 more sources
Subduction Initiation by Plume‐Plateau Interaction: Insights From Numerical Models
It has recently been demonstrated that the interaction of a mantle plume with sufficiently old oceanic lithosphere can initiate subduction. However, the existence of large lithospheric heterogeneities, such as a buoyant plateau, in proximity to a rising ...
Marzieh Baes +3 more
doaj +1 more source

