Results 91 to 100 of about 27,222 (235)
Morphology and tectonics of the Mid-Atlantic Ridge, 7°–12°S
We present swath bathymetric, gravity, and magnetic data from the Mid-Atlantic Ridge between the Ascension and the Bode Verde fracture zones, where significant ridge–hot spot interaction has been inferred.
Bijwaard +56 more
core +1 more source
Modeling pN2 through Geological Time: Implications for Planetary Climates and Atmospheric Biosignatures [PDF]
Nitrogen is a major nutrient for all life on Earth and could plausibly play a similar role in extraterrestrial biospheres. The major reservoir of nitrogen at Earth's surface is atmospheric N2, but recent studies have proposed that the size of this ...
Buick, R. +5 more
core +2 more sources
Computer program determines the radiant flux to the base region of a real gas system with an axisymmetric geometry and any axisymmetric property ...
De Soto, S., Vok, C. A.
core +1 more source
Thick Underplating and Buoyancy of the Bermuda Swell
Bermuda is an intraplate ocean swell that does not conform to traditional mantle plume theory. Unlike other prominent bathymetric swells, such as Hawaii, it lacks age‐progressive volcanism, a deeply rooted mantle plume, and modern volcanism.
William D. Frazer, Jeffrey Park
doaj +1 more source
The causes and global distribution of intraplate volcanism remain poorly understood, particularly the occurrence of scattered magmatism unrelated to large igneous provinces (LIPs).
X. Zhu, A. Balázs, T. Gerya, Z. Sun
doaj +1 more source
Coldspots or hotspots? The origin of plateau-shaped highlands on Venus [PDF]
A compelling question for the terrestrial planets is the origin of the highland regions on Venus. Data on the topography, gravity signature, and surface morphology returned by the Pioneer Venus, Venera 15/16, and Magellan spacecraft represent a basis for
Bindschadler, D. L.
core +1 more source
The evolution of the Galápagos mantle plume. [PDF]
Soderman CR +5 more
europepmc +1 more source
Abstract From oxic atmosphere to metallic core, the Earth's components are broadly stratified with respect to oxygen fugacity. A simple picture of reducing oxygen fugacity with depth may be disrupted by the accumulation of oxidised crustal material in the deep lower mantle, entrained there as a result of subduction. While hotspot volcanoes are fed by
Moussallam, Yves +9 more
openaire +5 more sources
Deep mantle plumes and an increasing Earth radius
Recent space geodetic and gravimetric studies have given indications that the Earth's radius is increasing at 0.1–0.4 mm yr−1 at present. Seismic studies have also shown that earthquakes alone could be causing the radius to increase at 0.011–0.06 mm yr−1.
Matthew R. Edwards
doaj +1 more source
On gravity from SST, geoid from Seasat, and plate age and fracture zones in the Pacific [PDF]
A composite map produced by combining 90 passes of SST data show good agreement with conventional GEM models. The SEASAT altimeter data were deduced and found to agree with both the SST and GEM fields. The maps are dominated (especially in the east) by a
Marsh, B. D. +2 more
core +2 more sources

