Results 71 to 80 of about 365,115 (188)

Crustal flow beneath Iceland [PDF]

open access: yes
Theoretical and experimental studies indicate that when oceanic crust is hotter than about 800°C, variations in crustal thickness drive lower crustal flow.
Maclennan, J., Jones, S. M.
core   +1 more source

Reappraising elastic thickness variation at oceanic trenches [PDF]

open access: yes
We reassess the variation of elastic thickness as a function of lithospheric plate age using a global database of bathymetric and free-air gravity profiles which are perpendicular to oceanic trenches.
White, N. J., Bry, M.
core   +1 more source

Structural and Morphologic Study of Shatsky Rise Oceanic Plateau in the Northwest Pacific Ocean from 2D Multichannel Seismic Reflection and Bathymetry Data and Implications for Oceanic Plateau Evolution [PDF]

open access: yes, 2015
Shatsky Rise is one of the largest oceanic plateaus, a class of volcanic features whose formation is poorly understood. It is also a plateau that was formed near spreading ridges, but the connection is unclear.
Zhang, Jinchang
core   +1 more source

Octopus insularis (Cephalopoda: Octopodidae) on the tropical coast of Brazil: where it lives and what it eats

open access: yesBrazilian Journal of Oceanography
Octopus insularis is the dominant octopus in the shallow tropical waters of the coast and oceanic islands in the North and Northeast of Brazil. Is the abundance, distribution, habitat and diet of this species on the continent the same as in oceanic ...
Allan Torrecilla Batista   +1 more
doaj   +1 more source

Tha datasets for Probing the world's largest oceanic plateau: From making to collision

open access: yes
<p>Tha seismic datasets for Probing the world's largest oceanic plateau: From making to collision</p ...
Liu, Hongwei   +6 more
core   +1 more source

Plume versus plate origin for the Shatsky Rise oceanic plateau (NW Pacific): Insights from Nd, Pb and Hf isotopes

open access: yes, 2014
Shatsky Rise, an early Cretaceous igneous oceanic plateau in the NWPacific, comprises characteristics that could be attributed to either formation by shallow, plate tectonic-controlled processes or to an origin by a mantle plume(head).
Romanova, Irina V.   +9 more
core   +1 more source

Decadal-Scale Warming Signals in Antarctic Ice Sheet Interior Revealed by L-Band Passive Microwave Observations from 2015 to 2025

open access: yesRemote Sensing
The Antarctic ice sheet, Earth’s largest ice mass, is vital to the global climate system. Analyzing its thermal behavior is crucial for sea-level projections and ice shelf assessments; however, internal temperature studies remain challenging due to the ...
Shaoning Lv, Yin Hu, Jun Wen
doaj   +1 more source

Sedimentary Markers of Ocean Plateau Volcanism during the Cretaceous Oceanic Anoxic Events

open access: yes, 2019
The Cretaceous Period saw numerous profoundenvironmental perturbations, including the Early Aptian(~120 Ma) and Cenomanian–Turonian (~94 Ma) OceanicAnoxic Events (OAEs). The causal mechanisms of theseOAEs remain debated, but were likely linked to large-scalevolcanic activity that occurred during the emplacement ofocean plateaus (e.g., Greater Ontong ...
Percival, Lawrence   +12 more
openaire   +2 more sources

Seismicity catalog from: Subduction of an oceanic plateau across southcentral Alaska: High-resolution seismicity

open access: yes
Please cite as: Daly, K. A., Abers, G. A., Mann, M.E., Roecker, S., & Christensen, D.H. (2026), Seismicity catalog from: Subduction of an oceanic plateau across southcentral Alaska: High-resolution seismicity.[dataset] Cornell University Library ...
Abers, Geoffrey A.   +4 more
core   +1 more source

Crustal fault reactivation facilitating lithospheric folding/buckling in the central Indian Ocean

open access: yes, 1996
High-quality, normal-incidence seismic reflection data confirm that tectonic deformation in the central Indian Ocean occurs at two spatial scales: whole lithosphere folding with wavelengths varying between 100 and 300 km, and compressional reactivation ...
Beekman, F.   +3 more
core   +1 more source

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