Results 71 to 80 of about 50,735 (203)
Beyond spreading rate: Controls on the thermal regime of mid-ocean ridges. [PDF]
Chen J, Olive JA, Cannat M.
europepmc +1 more source
Larval Dispersal: Vent Life in the Water Column [PDF]
Visually striking faunal communities of high abundance and biomass cluster around hydrothermal vents, but these animals don't spend all of their lives on the seafloor.
Diane K. Adams +2 more
doaj
Lava Geochemistry as a Probe into Crustal Formation at the East Pacific Rise [PDF]
Basalt lavas comprise the greatest volume of volcanic rocks on Earth, and most of them erupt along the world's mid-ocean ridges (MORs). These MOR basalts (MORBs) are generally thought to be relatively homogeneous in composition over large segments of the
Michael R. Perfit +8 more
doaj
Velocity sections of the upper mantle under the oceans
We constructed the models of the distribution of longitudinal seismic waves velocities for the upper mantle oceanic regions: mid-ocean ridges (MOR), basins, trenches, island arcs and coastal ridges, back-arc troughs (BAT).
V.V. Gordienko, L.Ya. Gordienko
doaj +1 more source
The spreading rate dependence of the distribution of axial magma lenses along mid-ocean ridges. [PDF]
Liu Z, Buck WR.
europepmc +1 more source
The Prediction, Verification, and Significance of Flank Jets at Mid-Ocean Ridges [PDF]
One aspect of ocean flow over mid-ocean ridges that has escaped much attention is the capacity of a ridge to convert oscillatory flows into unidirectional flows.
J. William Lavelle +4 more
doaj
The Lau Basin Float Experiment (LAUB-FLEX) [PDF]
Before 2004, little was known about deep ocean circulation in the Lau Basin, a semi-enclosed basin in the South Pacific Ocean, about 1,500 km north of New Zealand.
Kevin Speer, Andreas M. Thurnherr
doaj
Mid-Ocean Ridge Geochemistry and Petrology
false ; 2016-03-16T16:38 ...
unknown ( host institution ) +1 more
openaire +2 more sources
The Role of Peridotite for Oceanic Volcanism
The complementary products of oceanic crust formation are compositionally variable melt‐depleted peridotites. Together with the oceanic crust, the melt‐depleted peridotites are continuously recycled back into the mantle.
Andreas Stracke, Vincent J. M. Salters
doaj +1 more source
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait [PDF]
Methane expulsion from the world ocean floor is a broadly observed phenomenon known to be episodic. Yet the processes that modulate seepage remain elusive.
Bunz, Stefan +6 more
core +1 more source

